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SEAMA NobukazuGraduate School of Science / Division of PlanetologyProfessor
Researcher basic information
■ Research Keyword■ Research Areas
■ Committee History
- 2025 - Present, IODP3 (International Ocean Drilling Programme), MSP Facility Board, Co-Chair, https://iodp3.org/iodp3-organisation/iodp3-msp-facility-board/
- 2019 - Present, 地震・火山噴火予知研究協議会, 委員
- 2018 - Present, 日本地球惑星科学連合 固体地球科学セクション, ボードメンバー
- 2019 - 2024, Chikyu IODP Board (CIB), Chair
- 2018 - 2024, 日本地球掘削科学コンソーシアム, 理事
- 2015 - 2019, 海洋研究開発機構海洋工学センター, 助言委員会アドバイザー(委員)
- 2010 - 2015, 海洋研究開発機構海洋工学センター, 評価助言委員会アドバイザー (委員)
- 2008 - 2012, InterRidge Mantle Imaging WG, Chair
- 2005 - 2008, InterRidge(国際中央海嶺共同研究機構), Steering Committee委員
Research activity information
■ Award■ Paper
- Abstract We have developed a 3-D forward modeling method for the magnetometric resistivity (MMR) technique, specially focusing on the marine MMR method, which utilizes a vertical bipole source and seafloor receivers to measure magnetic field variations. The bipole source generates an artificial electric current between two electrodes: one on the sea surface and another on the seafloor. When computing the electric potential using the relaxation method, while conserving electric current, singularities arise at the electrode locations. To address this issue, we introduce two electrical resistivity structures to mitigate the effects of these singularities and to obtain magnetic field anomalies caused by arbitrary 3-D electrical resistivity anomalies beneath the seafloor. By determining the sign of the magnetic field anomaly, we can infer whether the electrical resistivity of the anomalous body is more conductive or more resistive compared to the surrounding oceanic crust. Furthermore, we demonstrate that increasing the number of bipole sources is more effective in exploring anomalous bodies than increasing the number of receivers. Graphical abstractSpringer Science and Business Media LLC, Oct. 2024, Earth, Planets and Space, 76(1) (1), 130[Refereed]Scientific journal
- Aug. 2024, Communications Earth & Environment, 5, 428[Refereed]Scientific journal
- Elsevier BV, Apr. 2024, Journal of Volcanology and Geothermal Research, 448, 108017 - 108017[Refereed]Scientific journal
- Abstract The Osaka Bay is situated at a seismically active region north of the Median Tectonic Line and east of Awaji Island in western Japan, known as part of the Kinki Triangle and the Niigata–Kobe Tectonic Zone. Dense distribution of active faults and high geodetic strain rates characterize the region, posing a major seismic hazard potential to the coastal and metropolitan areas of the Kansai region. To investigate the shallow structure and recent deformation history of active faults in the Osaka Bay, we acquired 15 high-resolution seismic profiles using a Mini-GI airgun and a Boomer as active sources, together with multi-beam bathymetry data across the Osaka Bay Fault. Our seismic sections image a ~ 0.1 to 3.7 km-wide asymmetric anticline forelimb above the Osaka Bay Fault at shallow depths, coupled with a ~ 2.6 km-wide syncline to the west, and a broad, ~ 11 km-wide syncline in the footwall to the east. The synclinal axial surface at shallow depths measured in this study ranges 75°–89°. We observe the vertical displacement of the Osaka Bay Fault increasing northwards along strike. The sediment thickness on the hanging wall, however, is variable, modified by non-tectonic processes such as by tidal currents, affecting the geometry of growth strata. The most recent deformation by the Osaka Bay Fault reaches to near the seafloor by active folding, with large vertical offsets of 8–14 m over the last ~ 11 ka, and 5–11 m over the last ~ 5 ka. By combining with previously reported borehole age data, the average uplift rate on the Osaka Bay Fault is estimated to be ~ 1.0 to 1.7 m/ka during the Latest Pleistocene to Holocene. The inferred slip of the Osaka Bay Fault during the Holocene is likely to account for > 5% of the regional geodetic strain accumulation within the Kinki Triangle. Further studies to evaluate the Holocene slip rates of regional faults are necessary to assess the seismic hazards and the internal strain budgets within the Kinki Triangle and the Niigata–Kobe Tectonic Zone. Graphical abstractSpringer Science and Business Media LLC, Feb. 2024, Progress in Earth and Planetary Science, 11(1) (1)[Refereed]Scientific journal
- Abstract Recent research has shown that shallow tremors tend to occur in spatial association with heterogeneous conditions, which are formed by seamounts or ridges on the subducted oceanic crust. In the southern Kuril Trench, shallow tremors have been observed on the western side, although no apparent heterogeneity in the subducted oceanic crust has been identified. To investigate structures spatially associated with these shallow tremors, we processed reflection seismic data acquired along seven profiles. We examined structures ranging from the seafloor to the top of the oceanic crust, within a depth of up to 20 km. Our results reveal that undulations observed at the top of the subducted oceanic crust are related to the distribution and number of shallow tremors. The undulations would play a crucial role in the distribution of shallow tremors.American Geophysical Union (AGU), Dec. 2023, Geophysical Research Letters, 51(1) (1)[Refereed]Scientific journal
- Elsevier BV, Feb. 2023, Journal of Volcanology and Geothermal Research, 434, 107738 - 107738[Refereed]Scientific journal
- Mar. 2022, Journal of Geophysical Research: Solid Earth, 127(3) (3), English[Refereed]Scientific journal
- Apr. 2021, Scientific Drilling, 29, 69 - 82, English[Refereed]Scientific journal
- Jul. 2018, Earth, Planets and Space, 70, 111, English[Refereed]Scientific journal
- Kikai submarine caldera to the south of the Kyushu Island, SW Japan, collapsed at 7.3 ka during the latest supereruption (>500 km3 of magma) in the Japanese Archipelago. Multi functional research surveys of the T/S Fukae Maru in this caldera, including multi-beam echosounder mapping, remotely operated vehicle observation, multi-channel seismic reflection survey, and rock sampling by dredging and diving, provided lines of evidence for creation of a giant rhyolite lava dome (~32 km3) after the caldera collapse. This dome is still active as water column anomalies accompanied by bubbling from its surface are observed. Chemical characteristics of dome-forming rhyolites akin to those of presently active small volcanic cones are different from those of supereruption. The voluminous post-caldera activity is thus not caused simply by squeezing the remnant of syn-caldera magma but may tap a magma system that has evolved both chemically and physically since the 7.3-ka supereruption.ネイチャー・ジャパン株式会社, Feb. 2018, Scientific Reports (Nature Publishing Group), 8(1) (1), 2753 - 2753, English, International magazine[Refereed]Scientific journal
- Jun. 2015, POLAR SCIENCE, 9(2) (2), 221 - 234, English[Refereed]Scientific journal
- Springer Japan, Jan. 2015, Subseafloor Biosphere Linked to Hydrothermal Systems: TAIGA Concept, 2015(XVIII) (XVIII), 215 - 227, English[Refereed]In book
- Springer Japan, Jan. 2015, Subseafloor Biosphere Linked to Hydrothermal Systems: TAIGA Concept, 2015(XVIII) (XVIII), 229 - 240, English[Refereed]In book
- Springer Japan, Jan. 2015, Subseafloor Biosphere Linked to Hydrothermal Systems: TAIGA Concept, 2015(XVIII) (XVIII), 241 - 251, English[Refereed]In book
- Springer Japan, Jan. 2015, Subseafloor Biosphere Linked to Hydrothermal Systems: TAIGA Concept, 2015(XVIII) (XVIII), 253 - 260, English[Refereed]In book
- Apr. 2014, GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 15(4) (4), 1580 - 1599, English[Refereed]Scientific journal
- Dec. 2013, GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 14(12) (12), 5286 - 5307, English[Refereed]Scientific journal
- 2013, EARTH PLANETS AND SPACE, 65(8) (8), 883 - 891, English[Refereed]Scientific journal
- Oct. 2012, GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 13(10) (10), Q10017, English[Refereed]Scientific journal
- Jun. 2011, EARTH AND PLANETARY SCIENCE LETTERS, 306(1-2) (1-2), 55 - 65, English[Refereed]Scientific journal
- Sep. 2010, GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 11(9) (9), Q09003, English[Refereed]Scientific journal
- Sep. 2010, Scientific Drilling, 10, 56-63(10) (10), 56 - 63, English[Refereed]Scientific journal
- Tokyo Geographical Society, 2009, Chigaku Zasshi (Jounal of Geography), 118(6) (6), 1037 - 1063, Japanese[Refereed]Scientific journal
- Mar. 2008, EXPLORATION GEOPHYSICS, 39(1) (1), 52 - 59, English[Refereed]Scientific journal
- Jun. 2007, PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 162(1-2) (1-2), 2 - 12, English[Refereed]Scientific journal
- 2007, EARTH PLANETS AND SPACE, 59(8) (8), 981 - 986, EnglishA study on correction equations for the effect of seafloor topography on ocean bottom magnetotelluric data[Refereed]Scientific journal
- Apr. 2006, GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 7, English[Refereed]Scientific journal
- 海洋調査技術学会, 2006, Journal of Japan Society for Marine Surveys and Technology, 18(1), 17-27(1) (1), 17 - 27, JapaneseMeasurements by Ocean Bottom Gravimeter at Harima-nada in Seto Inland Sea, Japan.[Refereed]Scientific journal
- 2006, Butsuri-Tansa, 59(2), 171-180,, JapaneseSurveys of the oceanic crust resistivity structure using a Magnetometric Resistivity method[Refereed]
- Jul. 2005, Earth, Planets and Space, 57(7) (7), 673 - 677Scientific journal
- May 2005, Earth, Planets and Space, 57(5) (5), 465 - 470[Refereed]Scientific journal
- Surface geophysical, airgun-OBS (ocean bottom seismograph), and deep-towed surveys by R/V Kairei KR01-15 cruise, and OBS array observations were conducted to characterize geophysical features of a hydrothermal system in Suiyo Seamount as a part of Archaean Park Project. Geomagnetic results from surface and deep towed magnetometers suggest 1) the seamount was formed during Brunhes Epoch (after 0.78 My), and 2) a low magnetization area exists on its summit and is limited only on the eastern side with a diameter of 800 meters. 2-D ray tracing results, using four OBS data with a GI gun across the seamount in NE-SW direction, indicate that a P wave velocity of 2.2∿4.2 km s-1 (2 km thickness) is located all over the observation line. The OBS array observations reveal the seismic activity and the hypocenter determination indicates that the locations of these earthquakes are focused in a chimney-like shape within its diameter of 3 km just beneath the Suiyo volcanic cone at a depth of 3∿7km. We propose a model to explain these geophysical observations; the former main conduit of Suiyo Seamount is in the middle of cooling after the last eruption, and its heat drives the hydrothermal system in Suiyo Seamount. We perform a numerical simulation of a magma injection in the conduit with its diameter of 1 km and its cooling process has two different mechanisms; 1) a major hydrothermal circulation exists in the uppermost crust with P wave velocity of 2.2∿4.2 km s-1 (2 km thickness), suggesting a higher porosity region, and 2) thermal conduction is dominated in the deeper part. In the thermal conduction region, the existence of a cooling area inside and a heating area outside near the former main conduit leads to thermal differential stress, which is the cause of earthquakes below a depth of 3 km. This is a reasonable explanation of chimney-like shape hypocenter locations. The magma injection in the conduit with its diameter of 1 km has enough heat to drive hydrothermal circulation at least for a few hundreds years and the hydrothermal circulation is maintained for long times enough to make the low magnetization area with its diameter of 800 meters through the high alteration of the rock. This stable existence of the hydrothermal system in Suiyo Seamount would be an important factor to discuss regarding the origin and evolution of subsurface-vent biospheres, especially when the hydrothermal system has been isolated.The Oceanographic Society of Japan, 2005, 海の研究, 14(2), 139-150(2) (2), 139 - 150, Japanese[Refereed]Scientific journal
- Paleomagnetic intensity variation through marine magnetic anomalies could provide the finest time-depended information on plate tectonics. Rapid progress in the study of marine magnetic anomalies at the mid-ocean ridge area and developments in observation techniques have revealed a link between magnetic anomalies and paleomagnetic intensity variation. Combining recent high-resolution magnetic anomaly data from sea-bottom surveys and sediment-derived paleomagnetic intensity variations has played a key role in providing hope to the hypothesis attributing "tiny wiggle" in marine magnetic anomalies to the paleomagnetic field. However, this does not mean that the other competing hypothesis based on the variation of magnetic layer thickness instead of paleomagnetism, is ruled out. More data and higher analytic techniques would narrow down these possible sources. We introduce some significant steps to the evidences of the paleomagnetic field in magnetic anomalies along with history that sea-going geophysicists have piled up, including the development of instrument and magnetic structure models, and a shift in interpreting magnetic signals as geochemistry of the extrusive rocks, bathymetry expression, low-temperature alteration of basalt by fissuring and cracking, weathering by oxidation with age and the variation of magnetic layer thickness.Tokyo Geographical Society, 2005, 地学雑誌, 114(2)、239-249(2) (2), 239 - 249, Japanese[Refereed]Scientific journal
- The Archaean Park Project, which is funded by Special Coordination Fund of the Ministry of Education, Science and Technology (MEXT) is a major program to analyze the interaction between the sub-vent biosphere and the geosphere of the seafloor hydrothermal system. The convection of hydrothermal fluid within the oceanic crust gives rise to various sub-surface environments near hydrothermal vents. Such environmental conditions are analogous to the site of origin and/or early evolution of life during the Archaean age. Since the Domain Bacteria and Domain Archaea near the root of the Universal Tree are hyper-thermophilic, we named our proposal the "Archaean Park Project". There are four sub-themes in the project; 1) Physical processes of hydrothermal circulation systems, 2) Observation of the chemical environment of the sub-vent biosphere, 3) Microbiology and molecular ecology in the sub-vent biosphere; and 4) Interaction between microbial and geological processes. Here, we summarize the results of the research mainly performed in the first three-year period in terms of the deep-sea hydrothermal system at Suiyo Seamount, Izu-Bonin arc (Ogasawara arc), western Pacific.The Oceanographic Society of Japan, 2005, 海の研究, 14(2) (2), 129 - 137, Japanese[Refereed]Scientific journal
- Sep. 2004, MARINE GEOPHYSICAL RESEARCHES, 25(3-4) (3-4), 221 - 231, English[Refereed]Scientific journal
- 2004, Earth, Planets and Space, 56(2) (2), 217 - 227, English[Refereed]Scientific journal
- 2004, GEOCHEMICAL JOURNAL, 38(6) (6), 527 - 534, EnglishDiscovery of a new hydrothermal venting site in the southernmost Mariana Arc: Al-rich hydrothermal plumes and white smoker activity associated with biogenic methane[Refereed]Scientific journal
- Sep. 2003, GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 4, English[Refereed]Scientific journal
- 2003, Jour.Japan Soc.Mar.Surv.Tech., 15,71-87, Japanese海洋調査フロンティア増補版第5章-近年の海洋における地球物理観測技術の進歩Scientific journal
- Aug. 2002, GEOPHYSICAL JOURNAL INTERNATIONAL, 150(2) (2), 392 - 402, English, International magazine[Refereed]Scientific journal
- 2002, Journal of the Geological Society of Korea, 38(4) (4), 519 - 535Study on deep crustal structure of the Ulleung Basin, the East Sea (Japan Sea), from separating shallow components of gravity anomalies[Refereed]Scientific journal
- 2002, Antarctica at the close of a millennium, The Royal Society of New Zealand, 35, 539-547Basement orientation in the East Enderby Basin, Southern Indian Ocean[Refereed]
- Elsevier BV, Jan. 2000, Physics of the Earth and Planetary Interiors, 117(1-4) (1-4), 3 - 20Scientific journal
- Oct. 1999, Science, 286(5440) (5440), 752 - 756, English[Refereed]Scientific journal
- 1999, Journal of the Geological Society of Korea, 35, 297 - 308Constraints from magnetic anomalies on the structure of the Ulleung Basin, the East Sea (Japan Sea), using analytic signal and reduction to the pole transformations[Refereed]Scientific journal
- Nov. 1997, Science, 278(5341) (5341), 1281 - 1284, English[Refereed]Scientific journal
- Nov. 1996, Geophysical Research Letters, 23(23) (23), 3431 - 3434, English[Refereed]Scientific journal
- 1996, Geological Society Special Publication, 108, 265 - 273, English[Refereed]Scientific journal
- The Ayu Trough lies on the southern boundary between the Philippine Sea Plate and Caroline Plate. Although this trough may be the best place to study the evolution and kinematics of the Philippine Sea Plate, the origin and evolution of this trough are poorly understood. Our geophysical and morphological surveys in the northern part of the Ayu Trough revealed that the trough shares morphological similarities with slow‐spreading mid‐ocean ridges. The seafloor ages and an average spreading rate of the trough were inferred from the average length of the ridge segments, distribution of sediment thickness, and basement subsidence. Based on the seismic section at 3°30′N, the opening of the trough started about 25 Ma with an average half‐spreading rate 4.1 mm/yr. This spreading rate is much slower than some previous estimates. The present magma production rate and activity of the trough is estimated to be even lower than the 25 m.y. average. The seafloor depth of the trough axis and relief of the axial valley are approximately twice as deep as that of active mid‐ocean ridges. The trough axis valley is covered with sediment in contrast with the axial valleys of active mid‐ocean ridges. Sedimentation at the trough axis shows that the spreading rate has been quite slow for the last 2.5 Ma.American Geophysical Union (AGU), Jan. 1995, Geophysical Research Letters, 22(2) (2), 109 - 112[Refereed]Scientific journal
- 1995, Journal of the Geodetic Society of Japan, 41(1) (1), 75 - 89, English[Refereed]Scientific journal
- Society of Geomagnetism and Earth, Planetary and Space Sciences, 1994, Journal of geomagnetism and geoelectricity, 46(6) (6), 455 - 462[Refereed]
- Society of Geomagnetism and Earth, Planetary and Space Sciences, 1994, Journal of geomagnetism and geoelectricity, 46(7) (7), 571 - 586[Refereed]
- Society of Geomagnetism and Earth, Planetary and Space Sciences, 1993, Journal of geomagnetism and geoelectricity, 45(11) (11), 1383 - 1394[Refereed]
- 1993, Geopys. J. Int., 113, 155-164[Refereed]
- Elsevier BV, Apr. 1992, Earth and Planetary Science Letters, 109(3-4) (3-4), 347 - 354[Refereed]Scientific journal
- 1992, Journal of Japan Society of Marine Survey Technology, 4(2) (2), 41 - 49[Refereed]
- 1992, Recent Progress in Antarctic Earth Sciences, TERRAPUB, 649-654The directions of magnetic anomaly lineations in Enderby Basin, off Antarctica[Refereed]
- Magnetic survey in Ongul islandsTotal intensities of the geomagnetic field were measured in the eastern part of West Ongul Island and the southern part of East Ongul Island during the 30th Japanese Antarctic Research Expedition (JARE-30) in 1989. Measurements were carried out along two east-west observation lines in West Ongul Island and two east-west and three north-south observation lines in East Ongul Island. The variations of magnetic anomalies in West Ongul Island seem to correlate with the surface geology, while those in East Ongul Island do not. A model calculation showed a positive correlation of the obtained variations in West Ongul Island with the geological structure and the paleomagnetic results. However, widths and positions of the magnetic anomaly source model are slightly different from those of the surface geological structure. These differences provide information how the surface geological structure extends underground.National Institute of Polar Research, 1991, Proc. NIPR Symp. Antarct. Geosci., 5, 11 - 19, English[Refereed]
- Elsevier BV, Sep. 1990, Tectonophysics, 181(1-4) (1-4), 285 - 297[Refereed]Scientific journal
- Measurement of geomagnetic field at sea during JARE-30, 1988-1989第30次南極地域観測において, 船上地磁気3成分磁力計による地磁気3成分測定およびプロトン磁力計による地磁気全磁力測定の同時観測を行った。プロトン磁力計の全磁力測定から船速の違いによるノイズの変化が見られた。このノイズの変化は, 船速が速くなりセンサーが不安定になることによって引き起こされたと考えられる。船上地磁気3成分測定からは, 船の船首方位の細かな揺動による短波長のノイズが見られた。船上地磁気3成分測定によって得られた地磁気3成分のデータに, プロトン磁力計によって得られた全磁力の結果をうまく適合することによって, 地磁気3成分のデータの絶対値に関してより信頼度の高いデータが得られた。現段階では, 地磁気3成分のデータの絶対値に関する問題を扱う場合プロトン磁力計との同時観測が必要である。以上の結果をもとに, 今後の海上における地磁気測定の改善が望まれる。Three components and total intensity of the geomagnetic field were measured by STCM (Shipboard Three Components Magnetometer) and a proton magentometer at the same time at sea during the 30th Japanese Antarctic Research Expedition. The measurements of total intensity of the geomagnetic field by a proton magnetometer showed a variation of noises in harmony with the variation of ship's velocity. This variation of noises may be caused by instability of the sensor due to large velocity of the ship. The measurements of three components of the geomagnetic field by STCM revealed short wavelength noiscs which were caused by small yawing of the ship. Reliable absolute values of three components of the geomagnetic field were obtained by adapting the total intensity of the geomagnetic field measured by a proton magnetometer to the data of three components of the geomagnetic field measured by STCM. In the present state of STCM, it is necessary to measure three components and total intensity of geomagnetic field by STCM and a proton magnetometer simultaneously, in case of obtaining the absolute values of three components of the geomagnetic field. These results suggest that improvement of measurement of the geomagnetic field at sea will be required.1990, Antarctic Record, 34(3) (3), 34, 346-356 - 356, Japanese[Refereed]
- Preliminary report of three components of geomagnetic field measured on board the icebreaker Shirase during JARE-30Measurement of three components of geomagnetic field was carried out on board the icebreaker SHIRASE during the 30th Japanese Antarctic Research Expedition (JARE-30). Vector anomalies of geomagnetic field were obtained and the directions of magnetic lineations were determined from the vector anomalies. They are in good agreement with the results previously reported along the ship's tracks (e. g. ROYER et al. : Tectonophysics, 155,235,1988; ROYER and SANDWELL : J. Geophys. Res., 94,13755,1989), except for the Antarctic continental margin and the Enderby Basin. In the Antarctic continental margin, N-S trending magnetic structure that coincides with the Australian-Antarctic depression is detected between Australia and Antarctica and the local magnetic anomaly that seems to be caused by the Napier Complex appears between 50°E and 60°E along 63°S. Further, in the Enderby Basin around 60°S, N-S and NNE-SSW trending magnetic lineations which have never been reported before are detected. These results may suggest new constraints on the evolution of the Indian Ocean.National Institute of Polar Research, 1990, Proc. NIPR Symp. Antarct. Geosci., 4, 4, 191-200 - 200, English[Refereed]
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- Mar. 2022, 号外地球, 72, 30 - 39現実的なマントル掘削のシナリオ
- 2021, 日本地球惑星科学連合大会予稿集(Web), 2021Preliminary results of ocean bottom pressure observation around Kikai submarine caldera, SW Japan
- The Japan Institute of Marine Engineering, 01 Jan. 2021, Marine Engineering, 56(1) (1), 139 - 143, JapaneseIntroduction scientific journal
- Jun. 2010, Workshop Report, 1-67, EnglishThe MoHole: A Crustal Journey and Mantle Quest Workshop Report
- Jun. 2009, Thematic Review, 2,1-65, EnglishOceanic Crustal Structure and Formation: IODP and ODP Achievements November 2002 - December 2005Introduction scientific journal
- 2009, White paper for IODP New Ventures in Exploring Scientific Targets (INVEST), 1-5, EnglishRealistic Mohole using D/V ChikyuOthers
- Jan. 2009, -, 1-11, EnglishOn Board Report of the recovery of OBEM (Ocean Bottom Electro - Magnetometer) during the 27th Umitaka-maru Cruise, 1/December/2008 - 2/January /2009Others
- Aug. 2008, Bref compte rendu, 1-5, EnglishCampagne ESSRES – Tests magnétométriques – 19-26 juillet 2008Others
- 2008, -, 6-26/January /2008, 1-59, EnglishOn Board Report of the Hakuho-maru Cruise KH-07-4 Leg 2Others
- 2007, -, 26/November-2/December/2007, 1, EnglishOn Board Cruise Report of KR07-16 Kairei CruiseOthers
- 2006, 不明, 38741, EnglishOn Board Cruise Report of KR06-12 Kairei Cruise
- 2006, Conductivity Anomaly 研究会 2006 年論文集, 136 - 137, JapaneseMagnetometric Resistivity 法の磁場の3次元フォワード計算(その2)―比抵抗異常領域がつくる磁場の特徴―
- 実業公報社, 2004, 地質ニュース, 598 24-29(598) (598), 24 - 29, Japanese海底熱水系地下生物圏への地球物理学的アプローチ-地下生物圏の構造をどのように把握するか-
- 2003, JAMSTEC Journal of Deep Sea Research, 22, 22, 89-106 - 106Preliminary report of KR02-14 Kairei cruise
- Japan Society of Geoinformatics, 1987, Geological data processing, 1987(12) (12), 217 - 226
- Others, 朝倉書店, Apr. 2018, Japanese図説 地球科学の事典Scholarly book
- Mantle structure and flow patterns beneath active back-arc basins inferred from passive seismic and electromagnetic methods, American Geophysical Union, 2006, English, ISBN: 9780875904313Back-arc spreading systems : geological, biological, chemical, and physical interactions
- 第5章近年の海洋における地球物理観測技術の進歩 5.1コンプライアンス測定/5.2コントロールソースを用いた電気伝導度測定, 2004「海洋調査フロンティア 海を計測する -増補版-」
- 日本地球惑星科学連合2025年大会, May 2025MOWALL-CIR: マリーセレスト・トランスフォーム断層の総合調査- 白鳳丸KH-24-4 航海速報Oral presentation
- 2025年度大阪大学理学同窓会講演会, Apr. 2025海底から探る 固体地球のダイナミクス
- SGEPSS CA研究会 2024年度研究集会, Mar. 2025⻤界カルデラ⽕⼭海域での地下⽐抵抗構造Oral presentation
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- 海と地球のシンポジウム2024, Mar. 2025マリーセレストトランスフォーム断層を用いて海洋地殻の鉛直磁化構造を探る試みOral presentation
- 海と地球のシンポジウム2024, Mar. 2025マリアナトラフの発達史Poster presentation
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- 日本火山学会2024年度秋季大会, Oct. 2024グローバルトモグラフィーによる鬼界カルデラ周辺のP波速度構造Poster presentation
- 日本火山学会2024年度秋季大会, Oct. 2024地震波トモグラフィによる鬼界カルデラのマグマ供給系イメージングOral presentation
- PROGRAMME AND ABSTRACTS THE VOLCANOLOGICAL SOCIETY OF JAPAN, Oct. 2024, Japanese, The Volcanological Society of JapanCharacteristics of the Kikai-Akahoya and Kikai-Tozurahara eruption deposits from submarine coresPoster presentation
- 2024年度日本地球化学会 第71回年会, Sep. 2024国際深海科学掘削計画:地震発生帯掘削の総括と新プログラム IODP3[Invited]Invited oral presentation
- The 26th Electromagnetic Induction Workshop, Sep. 2024Estimation of 3-D resistivity structure under the Kikai submarine caldera volcanoOral presentation
- 26th EM Induction Workshop, Sep. 2024Advancing the Magnetometric Resistivity Method:3D Forward Modeling with the Relaxation Technique
- Goldschmidt2024 abstracts, Aug. 2024, Geochemical SocietyMagmatic evolution leading to multiple calderagenic eruptions at Kikai volcano, Southwest Japan
- 日本地球惑星科学連合2024年大会, May 2024海陸自然地震観測による鬼界カルデラの地震波速度構造Oral presentation
- 日本地球惑星科学連合2024年大会, May 20247300年前の鬼界アカホヤ噴火以降の海底溶岩ドーム直下のマグマ供給系の進化(続編)Oral presentation
- 日本地球惑星科学連合2024年大会, May 2024Tracing the Kikai volcano evolution from geochemical surveys of subaerial and submarine depositsPoster presentation
- 日本地球惑星科学連合2024年大会, May 2024地磁気異常データを用いたマリアナトラフの拡大過程Oral presentation
- 日本地球惑星科学連合2024年大会, May 2024最終氷期以降における大阪湾の音響層序と地殻変動Oral presentation
- 日本地球惑星科学連合2024年大会, May 2024Magma re-injection after the 7.3 ka Kikai-Akahoya eruption of the Kikai submarine caldera volcanoOral presentation
- 日本地球惑星科学連合2024年大会, May 20243-D resistivity structure under the Kikai submarine caldera volcano.Oral presentation
- International Symposium “Submarine caldera volcanoes”, Mar. 2024, 神戸, International conference3-D resistivity structure under the Kikai submarine caldera volcanoOral presentation
- International Symposium “Submarine caldera volcanoes”, Mar. 2024, 神戸, International conferenceSeismic velocity structure at Kikai submarine caldera deduced from amphibious passive seismic observationOral presentation
- International Symposium “Submarine caldera volcanoes”, Mar. 2024, 神戸, International conference7.3 ka Kikai-Akahoya eruption of the Kikai submarine caldera volcano and current sta-tus of magma re-injectionOral presentation
- International Symposium “Submarine caldera volcanoes”, Mar. 2024, 神戸, International conferenceMagma sources and variability at Kikai Caldera, SW Japan pre-, syn- and post cal-deragenic eruptionsOral presentation
- International Symposium “Submarine caldera volcanoes”, Mar. 2024, 神戸, International conferenceMagma evolution from Tozurahara to Akahoya catastrophic eruptions at Kikai Caldera; a study on marine tephras from the Chikyu SCORE corePoster presentation
- 海と地球のシンポジウム2023, Mar. 2024, 口頭, 東京, Domestic conference鬼界カルデラ火山海域での地下比抵抗構造Oral presentation
- 日本地震学会2023秋季大会, Nov. 2023, 口頭, 横浜, Domestic conference北海道沖千島海溝での浅部微動分布に相関する構造Oral presentation
- 日本火山学会2023年度秋季大会, Oct. 2023, Domestic conference海陸自然地震観測による鬼界カルデラの地震波速度構造Poster presentation
- 日本火山学会2023年度秋季大会, Oct. 2023, Domestic conference鬼界カルデラのマグマ源とその進化Poster presentation
- 日本火山学会2023年度秋季大会, Oct. 2023, Domestic conference鬼界カルデラの海底カルデラ壁における掘削Oral presentation
- 地球電磁気・地球惑星圏学会2023年秋季年会, Sep. 2023, 口頭, 仙台, Domestic conference鬼界カルデラ火山海底下の三次元比抵抗構造解析Oral presentation
- 日本地質学会第130年学術大会, Sep. 2023, 口頭, 京都, Domestic conferenceサブボトムプロファイラーデータによって明らかになった大阪湾における小断層の分布と沖積層の音響層序区分Oral presentation
- International Joint Workshop on Slow-to-Fast Earthquakes 2023, Sep. 2023, Poster, 東京・オンライン, International conferenceShallow fault-related folding and late Quaternary slip rate of the Osaka Bay Fault, western JapanPoster presentation
- 日本地球惑星科学連合2023年大会, May 2023, 口頭, 千葉・オンライン, Domestic conference鬼界海底カルデラ火山の集中的な調査研究[Invited]Invited oral presentation
- 日本地球惑星科学連合2023年大会, May 2023, 口頭, 千葉・オンライン, Domestic conference7300年前の鬼界アカホヤ噴火以降の海底溶岩ドーム直下マグマ供給系の進化Oral presentation
- 日本地球惑星科学連合2023年大会, May 2023, 口頭, 千葉・オンライン, Domestic conference屈折法地震探査によって明らかになった鬼界カルデラ海底火山地下の低速度異常Oral presentation
- 日本地球惑星科学連合2023年大会, May 2023, 口頭, 千葉・オンライン, Domestic conferenceResistivity structure of the Lau basin as inferred from M2 tidal magnetic variation at the seafloorOral presentation
- Japan Geoscience Union Meeting 2023, May 2023, Poster, 千葉・オンライン, Domestic conferenceInvestigating the formation of the Kikai submarine lava dome using matrix glass volatile contentsPoster presentation
- 日本地球惑星科学連合2023年大会, May 2023, 口頭, 千葉・オンライン, Domestic conferenceImaging 3D resistivity structure under the seafloor of Kikai caldera volcanoOral presentation
- 海と地球のシンポジウム2022, Mar. 2023, Japanese, 東京, Domestic conference鬼界海底カルデラの総合調査Oral presentation
- 海と地球のシンポジウム2022, Mar. 2023, Japanese, 東京, Domestic conference屈折法地震波構造探査によって明らかになった鬼界カルデラ火山直下の低速度領域Oral presentation
- 海と地球のシンポジウム2022, Mar. 2023, Japanese, 東京, Domestic conference鬼界カルデラ火山海底下の三次元比抵抗構造解析Oral presentation
- 海と地球のシンポジウム2022, Mar. 2023, Japanese, 東京, Domestic conference鬼界カルデラ破局噴火のマグマ準備過程Oral presentation
- 地球電磁気・地球惑星圏学会2022年秋学会, Nov. 2022ラウ海盆における潮汐起因磁場の3D順計算
- 地球電磁気・地球惑星圏学会2022年秋学会, Nov. 2022, Japanese, 神奈川, Domestic conference海底地形効果を考慮した3次元比抵抗構造解析手法の開発Oral presentation
- 日本地震学会2022年度秋季大会, Oct. 2022, Japanese, 札幌, Domestic conference北海道沖千島海溝沈み込み帯における海底谷を挟んだ構造差とプレート間すべりの関係Oral presentation
- 日本地震学会2022年度秋季大会, Oct. 2022, Japanese, 札幌, Domestic conference屈折法地震波探査による鬼界カルデラ地下の地震波速度構造の推定Oral presentation
- 日本火山学会2022年度秋季大会, Oct. 2022, Japanese, 静岡・オンライン, Domestic conference屈折法地震波探査によって推定された鬼界カルデラ地下の地震波速度構造Oral presentation
- 2022年度 日本地球化学会 第69回年会, Sep. 2022, Japanese, 高知・オンライン, Domestic conference海底掘削試料から明らかになった鬼界カルデラ火山噴出物の特徴[Invited]Oral presentation
- 2022年度 日本地球化学会 第69回年会, Sep. 2022, Japanese, 高知・オンライン, Domestic conference鬼界カルデラ破局噴火の噴火準備過程―ちきゅうSCORE試料よりーOral presentation
- 日本地球惑星科学連合2022年大会, Jun. 2022, Japanese, 千葉・オンライン, Domestic conference鬼界海底カルデラにおける海陸自然地震観測Poster presentation
- 日本地球惑星科学連合2022年大会, May 2022, Japanese, 千葉・オンライン, Domestic conferenceInvestigation of subaerial and submarine deposits of pyroclastic density currents: A case study at Kikai volcano, SW JapanOral presentation
- 日本地球惑星科学連合2022年大会, May 2022, Japanese, 千葉・オンライン, Domestic conference反射法地震探査データによる北海道沖千島海溝前弧の地下構造Oral presentation
- Japan Geoscience Union Meeting 2022, May 2022, Japanese, Chiba / Online, Domestic conferenceInvestigating the formation of the Kikai submarine lava dome using matrix glass volatile contentsOral presentation
- 日本地球惑星科学連合2022年大会, May 2022, Japanese, 千葉・オンライン, Domestic conferenceLate Pleistocene to Holocene dynamic basin environment at the Osaka Bay: Stratigraphic expressions of tectonic deformation, sea level fluctuation, and tidal wavesOral presentation
- InterRidge-Japan研究集会, Nov. 2021フラクチャーゾーンとその周辺における海洋性地殻の形成と変遷
- SGEPSS 第 149 回総会・講演会, Nov. 2021フラクチャーゾーンとその周辺における海洋性地殻の形成と変遷
- 日本地球惑星科学連合2021年大会, Jun. 2021, オンライン鬼界アカホヤ噴火噴出物の陸上及び海底堆積物の対比
- 日本地球惑星科学連合2021年大会, Jun. 2021, オンラインShallow structure and late Quaternary slip rate on the Osaka Bay Fault: Aspects of climate-tectonic interaction
- 日本地球惑星科学連合2021年大会, Jun. 2021, オンライン薩摩半島南方における海底地すべりを起因とする堆積構造
- 日本地球惑星科学連合2021年大会, Jun. 2021, オンライン鬼界カルデラ・アカホヤ噴火による水中火砕堆積物の堆積様式
- 日本地球惑星科学連合2021年大会, Jun. 2021, オンラインDrilling of Kikai caldera volcano for elucidation of magma plumbing system and flow-deposition processes of large ignimbrite[Invited]
- 日本地球惑星科学連合2021年大会, Jun. 2021, オンライン重力異常から推定される鬼界カルデラ周辺の地殻構造
- 日本地球惑星科学連合2021年大会, Jun. 2021, オンライン鬼界海底カルデラ付近で得られた海底圧力観測の初期的な結果
- 日本地球惑星科学連合2021年大会, Jun. 2021, オンラインラウ海盆における潮汐起因磁場変動の一次元順計算:計算結果と海底磁場データ の比較および比抵抗構造に対する感度について
- 日本地球惑星科学連合2021年大会, Jun. 2021, オンライン地形効果を含む海底MTデータを扱う3次元インバージョンコードの開発 ~フォワード問題に関して~
- 日本地球惑星科学連合2021年大会, Jun. 2021, オンラインMagnetic and gravity constraints on crustal structure of the Nosappu Fracture Zone, Northwestern Pacific
- 海と地球のシンポジウム2020, Dec. 2020鬼界海底カルデラ火山における地球物理学的観測及び地質岩石学的調査Oral presentation
- 海と地球のシンポジウム2020, Dec. 2020鬼界海底巨大カルデラ火山における二重カルデラ形成過程の解明―新青丸 KS-19-17 航海概要報告―Oral presentation
- JpGU-AGU joint Meeting 2020, May 2020, EnglishAn overview of volcanic rocks from submarine Kikai CalderaOral presentation
- JpGU-AGU joint Meeting 2020, May 2020, EnglishPreliminary report of marine sediments drilled and cored by D/V Chikyu at Kikai volcano, SW JapanOral presentation
- JpGU-AGU joint Meeting 2020, May 2020, JapaneseSeismic facies and distribution of submarine pyroclastic depositsoriginated from multiple large-scale eruptions of Kikai calderaOral presentation
- JpGU-AGU joint Meeting 2020, May 2020, EnglishPre-prososal 951: The middle aged upper crust penetration on theNorth Arch off-Hawaii MoHole candidate siteOral presentation
- JpGU-AGU joint Meeting 2020, May 2020, EnglishShort to long term morphological changes and migration of sandwaves in a semi-enclosed sea: a case study in Okinose area of OsakaBayOral presentation
- JpGU-AGU joint Meeting 2020, May 2020, JapaneseStructure of submarine mass-transport complexes(MTCs) southernMt.KaimonOral presentation
- JpGU-AGU joint Meeting 2020, May 2020, EnglishDistribution of the volcanic rock around Kikai caldera submarine volcano, estimated from the geomagnetic anomaliesOral presentation
- JpGU-AGU joint Meeting 2020, May 2020, EnglishHow fracture zones work on subducting lithosphere?Poster presentation
- American Geophysical Union(AGU) Fall Meeting 2019, Dec. 2019, San Francisco, International conferenceFlow and depositional processes of the Koya Pyroclastic Flow formed by the Kikai caldera-forming eruption at 7.3 kaOral presentation
- InterRidge-Japan研究集会:海洋地殻-マントルの新たな実像:オマーン掘削から、海域観測から, Nov. 2019, 東京大学大気海洋研究所, Domestic conferenceGeomagnetic paleointensity variation during the Cretaceous Normal SuperchronPoster presentation
- InterRidge-Japan研究集会:海洋地殻-マントルの新たな実像:オマーン掘削から、海域観測から, Nov. 2019, 東京大学大気海洋研究所, Domestic conferenceThe structure of Submarine landslide at Mt. Kaimon offshorePoster presentation
- InterRidge-Japan研究集会:海洋地殻-マントルの新たな実像:オマーン掘削から、海域観測から, Nov. 2019, 東京大学大気海洋研究所, Domestic conferenceMagnetic anomalies around Kikai caldera submarine volcanoOral presentation
- InterRidge-Japan研究集会:海洋地殻-マントルの新たな実像:オマーン掘削から、海域観測から, Nov. 2019, 東京大学大気海洋研究所, Domestic conferenceGoverning factors of the mode of plate spreading that determine the oceanic crust architecture -the middle-aged upper crust drilling project Off-Hawaii-Oral presentation
- InterRidge-Japan研究集会:海洋地殻-マントルの新たな実像:オマーン掘削から、海域観測から, Nov. 2019, 東京大学大気海洋研究所, Domestic conferenceIntegrated study on submarine super-eruption, Kikai calderaOral presentation
- InterRidge Theoretical Institute 2019 ‘Hydrothermalism in 4D', Nov. 2019, Banyuls-sur-mer, France, International conferenceBasin scale water circulation inferred from geophysical evidences and numerical modelling[Invited]Keynote oral presentation
- 日本火山学会2019年度秋季大会, Sep. 2019, 神戸大学, Domestic conference幸屋火砕流の発生・流動様式Oral presentation
- 日本鉱物科学会2019年年会, Sep. 2019, 九州大学 伊都キャンパス, Domestic conference海洋地殻構造が示すプレート拡大モードの解明 -ハワイ沖モホール候補地における上部海 洋地殻貫通計画Oral presentation
- International Workshop on Western Pacific Marginal Sea Geodynamics, Jul. 2019, English, Tongji University, Shanghai, China, International conferenceAsymmetric seafloor spreading in back-arc basins: Evidences from the Southern Mariana back-arc basin[Invited]Invited oral presentation
- Japan Geoscience Union Meeting 2019, May 2019, Japanese, Makuhari Messe, Chiba, Domestic conferenceMigration of sand waves observed in Okinose area of Osaka BayOral presentation
- Japan Geoscience Union Meeting 2019, May 2019, Japanese, Makuhari Messe, Chiba, Domestic conferenceAn investigation of three-dimensional electrical resistivity structure under Kikai CalderaOral presentation
- Japan Geoscience Union Meeting 2019, May 2019, Japanese, Makuhari Messe, Chiba, Domestic conference鬼界カルデラ・アカホヤ噴火の水中火砕流の分布Oral presentation
- Japan Geoscience Union Meeting 2019, May 2019, Japanese, Makuhari Messe, Chiba, Domestic conferenceThe Analysis of magnetotelluric sounding data on Kikai submarine calderaOral presentation
- Japan Geoscience Union Meeting 2019, May 2019, Japanese, Makuhari Messe, Chiba, Domestic conferenceInvestigating Origin of landslide-like bathymetric feature at southernMt.Kaimon using bathymetric and multichannel seismic reflectionsurveysPoster presentation
- Japan Geoscience Union Meeting 2019, May 2019, Japanese, Makuhari Messe, Chiba, Domestic conferenceIdentification of submarine volcanic ash around the Kikai caldera with the Koya pyroclastic flow deposit inferred from glass compositionOral presentation
- Japan Geoscience Union Meeting 2019, May 2019, Japanese, Makuhari Messe, Chiba, Domestic conferenceSummary of Kikai submarine caldera researches conducted by KOBEC(Kobe Ocean-Bottom Exploration Center)Oral presentation
- Japan Geoscience Union Meeting 2019, May 2019, Japanese, Makuhari Messe, Chiba, Domestic conferenceThe Cretaceous Normal Superchron: records from the Pacific, Indian and Atlantic oceanic crustOral presentation
- Japan Geoscience Union Meeting 2019, May 2019, Japanese, Makuhari Messe, Chiba, Domestic conferencePreliminary report of the sea floor survey by a remotely operatedvehicle (ROV) at the Kikai caldera, SW JapanOral presentation
- 地球電磁気・地球惑星圏学会 第144回総会及び講演会, Nov. 2018, Japanese, Domestic conference南部マリアナ背弧拡大海嶺下の上部マントル比抵抗構造の解明Poster presentation
- 日本地球惑星科学連合2018年大会, May 2018, Japanese, 幕張メッセ, Domestic conference背弧海盆の非対称拡大を説明する仮説:南マリアナトラフでの観測事実と数値シミュレーションOral presentation
- Japan Geoscience Union Meeting 2018, May 2018, Japanese, Makuhari Messe, Chiba, Domestic conferenceThe characteristics of seismic stratigraphic facies of Kikai submarine caldera and off the southern KyusyuOral presentation
- Japan Geoscience Union Meeting 2018, May 2018, English, Makuhari Messe, Chiba, International conferenceThe significance of the surface excavation in the Kikai caldera, southern KyushuOral presentation
- Japan Geoscience Union Meeting 2018, May 2018, English, Makuhari Messe, Chiba, International conferenceSeafloor electromagnetic investigations of the upper mantle of the Mariana back-arc spreading and subduction systemPoster presentation
- Japan Geoscience Union Meeting 2018, May 2018, Japanese, Makuhari Messe, Chiba, Domestic conferenceIntegrated marine investigations of Kikai Caldera, SW JapanOral presentation
- 太平洋アレイ, Feb. 2018, Japanese, 東京大学地震研究所, Domestic conference背弧海盆の非対称拡大とその要因:南マリアナトラフでの観測事実と数値シミュ レーションOral presentation
- American Geophysical Union 2017 Fall Meeting, Dec. 2017, English, New Orleans, USA, International conferenceEnhanced and asymmetric melting beneath the southern Mariana back-arc spreading ridge under the influence of the Pacific plate subductionPoster presentation
- InterRidge-Japan研究集会, Nov. 2017, Japanese, 東京大学大気海洋研究所, Domestic conference背弧海盆の非対称拡大はどのようにして起こるのか?-南マリアナトラフでの観測事実と数値シミュレーション-Oral presentation
- InterRidge-Japan研究集会, Nov. 2017, Japanese, 東京大学大気海洋研究所, Domestic conferenceトランスフォーム断層における地磁気異常の要因の推定Poster presentation
- JpGU-AGU Joint Meeting 2017, May 2017, Japanese, 幕張メッセ, International conference伊豆・小笠原・マリアナ弧の背弧海盆で見られる2種類の上部海洋地殻地震波速度構造Oral presentation
- JpGU-AGU Joint Meeting 2017, May 2017, Japanese, 幕張メッセ, International conferenceTectonics of long-offset oceanic transform faults along the Central Indian RidgePoster presentation
- JpGU-AGU Joint Meeting 2017, May 2017, English, 幕張メッセ, International conferenceIntegrated offshore investigations in the vicinity of Kikai Caldera, southwestern Japan -towards a comprehensive understanding of destructive caldera eruptions-Oral presentation
- JpGU-AGU Joint Meeting 2017, May 2017, English, 幕張メッセ, International conferenceGeomorphological features of the Southern Mariana Trough spreading center obtained from near-bottom surveys using the AUV UrashimaPoster presentation
- JpGU-AGU Joint Meeting 2017, May 2017, English, 幕張メッセ, International conferenceAlong-trough variation in the seismic structure of the incoming Philippine Sea plate just seaward of the Nankai TroughPoster presentation
- Collaboration Research in global ocean and subduction, Apr. 2017, English, Seoul National University, International conferenceMantle heterogeneity beneath the Mariana Trough Back-Arc BasinOral presentation
- 海半球観測研究センター20周年シンポジウム「新たな観測が開く海半球の未来」, Mar. 2017, Japanese, 地震研究所, Domestic conference南東インド洋海嶺近傍における上部マントル比抵抗構造の推定Poster presentation
- 太平洋アレイ(PA)研究会, Sep. 2016, Japanese, 東京大学地震研究所, Domestic conference海洋底科学としての太平洋アレイOral presentation
- 23rd Electromagnetic Induction Workshop, Aug. 2016, English, The Empress Convention Center, International conferenceEnhanced and asymmetric melting beneath the southern Mariana back-arc spreading ridge, influenced by the subduction of the Pacific platePoster presentation
- 23rd Electromagnetic Induction Workshop, Aug. 2016, English, The Empress Convention Center, International conferenceElectrical resistivity structure under the western Cosmonauts Sea at the continental margin of East Antarctica inferred via a marine magnetotelluric experimentPoster presentation
- 23rd Electromagnetic Induction Workshop, Aug. 2016, English, The Empress Convention Center, International conferenceElectrical resistivity signature of the oceanic crust around hydrothermal vent sites on East Pacific Rise at 9° 50’NOral presentation
- 日本地球惑星科学連合2016年大会, May 2016, Japanese, 幕張メッセ, Domestic conference太平洋プレートの沈み込みの影響を受けた南部マリアナ背弧拡大海嶺下の豊富で非対称な部分溶融Oral presentation
- 日本地球惑星科学連合2016年大会, May 2016, Japanese, 幕張メッセ, Domestic conferenceフラクチャーゾーン、トランスフォーム断層を横切る深海地磁気調査Oral presentation
- 日本地球惑星科学連合2016年大会, May 2016, Japanese, 幕張メッセ, Domestic conferenceKH-15-5 白鳳丸研究航海速報:長大トランスフォーム断層と海嶺活動 CIR13°-18°SPoster presentation
- 東京大学地震研究所共同利用研究集会, Nov. 2015, Japanese, 東京大学地震研究所, Domestic conference沈み込む海洋プレートの違い:新しい視点Oral presentation
- 日本地震学会2015年度秋季大会, Oct. 2015, Japanese, Domestic conference海底地震観測による2011年東北地震北部震源域の余震分布Poster presentation
- 2nd InterRidge Workshop: Circum Antarctic Ridges, Oct. 2015, English, Korea Polar Research Institute, International conferenceReview of Japanese geophysical surveys of Indian Ocean RidgesOral presentation
- Third InterRidge Theoretical Institute Magmatic and Tectonic Processes and Seabed Resources at Mid-Ocean Ridges, Sep. 2015, English, Hangzhou, China, International conferenceReview of Japanese Taiga project 3, Southern MarianaTrough back-arc basin[Invited]Invited oral presentation
- 日本地球惑星科学連合2015年大会, May 2015, Japanese, 幕張メッセ国際会議場, Domestic conferenceWater release from subducting slab inferred by uppermantle electrical resistivity structures beneath back-arc basinsOral presentation
- 日本地球惑星科学連合2015年大会, May 2015, Japanese, 幕張メッセ国際会議場, Domestic conferenceDetermining the three-dimensional position of theanomalous resistivity body in upper oceanic crust using MMR methodOral presentation
- 日本地球惑星科学連合2015年大会, May 2015, Japanese, 幕張メッセ国際会議場, Domestic conferenceElectrical resistivity structure of the oceanic crust around hydrothermal vent sites on East Pacific Rise at N9 50'Oral presentation
- ブルーアース2015, Mar. 2015, Japanese, 独立行政法人海洋研究開発機構, 東京海洋大学(品川キャンパス), Domestic conferenceノサップフラクチャーゾーンにおける重力・地磁気・海底地形調査の概要Poster presentation
- Structure and Dynamics of the Oceanic Lithosphere/Asthenosphere System, Mar. 2015, English, the Normal Oceanic Mantle Project, Hotel Matsushima Taikanso, Miyagi, Japan, International conferenceUpper mantle electrical resistivity structures beneath the Indian Ocean and back-arc basinsPoster presentation
- 日本地震学会秋季大会, Nov. 2014, Japanese, Domestic conference福島県相馬沖の地震波速度構造調査Poster presentation
- AOGS 2014, Jul. 2014, English, Sapporo, International conferenceHydrothermal Heat Mining Due to the Aquifer Thickening Toward the Trench Axis: A Model for Explaining High Heat-flow Anomalies on the Seaward Side of the Japan TrenchPoster presentation
- 日本地球惑星科学連合2014年大会, May 2014, Japanese, パシフィコ横浜, Domestic conferenceElectrical resistivity structure of the Snail site at the Southern Mariana Trough spreading centerPoster presentation
- 日本地球惑星科学連合2014年大会, May 2014, Japanese, パシフィコ横浜, Domestic conferenceHydrothermal heat mining due to the aquifer thickening toward the trench axis: A model for the Japan TrenchOral presentation
- 日本地球惑星科学連合2014年大会, Apr. 2014, Japanese, パシフィコ横浜, Domestic conferenceHeterogeneity from mantle to crust at the central Southwest Indian Ridge(2)-Crust-Invited oral presentation
- 日本地球惑星科学連合2014年大会, Apr. 2014, Japanese, パシフィコ横浜, Domestic conferenceHeterogeneity from mantle to crust at the central Southwest Indian Ridge(1)-Upper mantle-Oral presentation
- 日本地球惑星科学連合2014年大会, Apr. 2014, Japanese, パシフィコ横浜, Domestic conferenceUpper mantle electrical resistivity structure at the continental margin of East AntarcticaPoster presentation
- ブルーアース2014, Feb. 2014, Japanese, 東京海洋大学品川キャンパス, Domestic conference南マリアナトラフ背弧海盆の海底拡大系における地球物理学調査Oral presentation
- ブルーアース2014, Feb. 2014, Japanese, 東京海洋大学品川キャンパス, Domestic conferenceQUELLE2013航海報告-Quest 1:インド洋Oral presentation
- 海底拡大系の総合研究:現状と将来 -InterRidge-Japan研究集会-, Nov. 2013, Japanese, 東京大学大気海洋研究所, Domestic conferenceSeismic structure and seismicity around the hydrothermal area in the Souther Mariana TroughOral presentation
- “Mid-ocean ridges and hydrothermal activity in the Indian Ocean” joint-hosted by Japan-Korea Marine Geoscience Symposium on Global Open Ocean Studies, Nov. 2013, English, 東京大学大気海洋研究所, International conferenceUpper mantle electrical resistivity structure beneath the Southwest Indian Ridge 37ºOral presentation
- “Mid-ocean ridges and hydrothermal activity in the Indian Ocean” joint-hosted by Japan-Korea Marine Geoscience Symposium on Global Open Ocean Studies, Nov. 2013, English, 東京大学大気海洋研究所, International conferenceGeophysical investigations of Rodriguez Triple Junction and southern Mariana Trough back-arc basinOral presentation
- 地球電磁気・地球惑星圏学会第134回総会・講演会, Nov. 2013, Japanese, 高知大学, Domestic conferenceElectrical resistivity structure under the Cosmonauts Sea offshore East AntarcticaPoster presentation
- 日本地球惑星科学連合2013年大会, May 2013, Japanese, 幕張メッセ, Domestic conferenceGeophysical results of the Southern Mariana Trough back-arc basin: From mantle to hydrothermal vent sitesOral presentation
- 日本地球惑星科学連合2013年大会, May 2013, Japanese, 日本地球惑星科学連合, 幕張メッセ, Domestic conferenceThermal subduction-zone model including hydrothermal circulation in an aquifer that thickened toward the trench axisOral presentation
- 21世紀の人間活動と資源,環境に関連した地球科学に関するシンポジウム, May 2013, Japanese, 東京大学理学部小柴ホール, Domestic conferenceマルチスケールで見た海底拡大系Oral presentation
- 日本地球惑星科学連合2013年大会, May 2013, Japanese, 幕張メッセ, Domestic conferenceTectonic background of a unique hydrogen-rich Kairei Hydrothermal Field, Central Indian Ridge: Results from Taiga ProjecOral presentation
- 2012 AGU Fall Meeting, Dec. 2012, English, AGU, San Francisco, USA, International conferenceUpper mantle electrical resistivity structure beneath the Southwest Indian Ridge 37°EPoster presentation
- 2012 AGU Fall Meeting, Dec. 2012, English, AGU, San Francisco, USA, International conferenceMantle to hydrothermal vent sites of the Southern Mariana Trough back-arc Basin: Results from the Taiga ProjectOral presentation
- 2012 AGU Fall Meeting, Dec. 2012, English, AGU, San Francisco, USA, International conferenceElectrical resistivity structure of the upper mantle in the Southern Mariana TroughPoster presentation
- 2012年地磁気・古地磁気・岩石磁気夏の学校, Sep. 2012, Japanese, 地磁気・古地磁気・岩石磁気研究会, 兵庫県立但馬長寿の郷,兵庫, Domestic conference最近の海底拡大系の地球物理学的知見と海底に眠る磁化構造・古地磁気の課題Invited oral presentation
- 日本地球惑星科学連合2012年大会, May 2012, Japanese, 日本地球惑星科学連合, 幕張メッセ,千葉, Domestic conference南マリアナトラフ拡大軸にある海底熱水系下の比抵抗構造推定Poster presentation
- 日本地球惑星科学連合2012年大会, May 2012, Japanese, 日本地球惑星科学連合, 幕張メッセ,千葉, Domestic conference南マリアナトラフにおける上部マントルの比抵抗構造Poster presentation
- 日本地球惑星科学連合2012年大会, May 2012, Japanese, 日本地球惑星科学連合, 幕張メッセ,千葉, Domestic conference中部マリアナ背弧拡大軸下のマントル溶融域に対する電磁気学的な制約Oral presentation
- 日本地球惑星科学連合2012年大会, May 2012, Japanese, 日本地球惑星科学連合, 幕張メッセ,千葉, Domestic conferenceラウ背弧海盆下の比抵抗構造の推定Oral presentation
- Mariana Vent Larvae (MarVel) Workshop: International Study of Connectivity Between Hydrothermal Vents, May 2012, English, Mariana Vent Larvae, Okinawa,Japan, International conferenceTectonic evolution, magmatic activity variation, and mantle dynamics of Mariana Trough back-arc basinInvited oral presentation
- The First Korea-Japan Marine Gepsciences Symposium, Apr. 2012, English, Seoul,Korea, International conferenceElectrical resistivity structural images beneath sea-floor spreading centersOral presentation
- ブルーアース2012, Feb. 2012, Japanese, 海洋研究開発機構, 東京海洋大学,東京, Domestic conference深海底熱水活動域に生息する化学合成微生物の遺伝学的多様性と群集構造の解明Poster presentation
- 2011 AGU Fall Meeting, Dec. 2011, English, AGU, San Francisco, USA, International conferenceUpper mantle electrical resistivity structure beneath back-arc spreading centersOral presentation
- 2011 AGU Fall Meeting, Dec. 2011, English, AGU, San Francisco, USA, International conferenceConstraint on a melting regime in upper mantle beneath the central Mariana back-arc spreading center through the geophysical electromagnetic forward modelingPoster presentation
- 地球電磁気・地球惑星圏学会第130回総会・講演会, Nov. 2011, Japanese, 地球電磁気・地球惑星圏学会, 神戸大学,兵庫, Domestic conference南マリアナトラフ拡大軸にある海底熱水系下の電気伝導度構造Oral presentation
- 地球電磁気・地球惑星圏学会第130回総会・講演会, Nov. 2011, Japanese, 地球電磁気・地球惑星圏学会, 神戸大学,兵庫, Domestic conferenceラウ背弧海盆下の2次元比抵抗構造の推定Oral presentation
- 日本地震学会2011年度秋季大会, Oct. 2011, Japanese, 日本地震学会, 静岡県コンベンションアーツセンター・グランシップ,静岡, Domestic conference沈み込む前後の地殻で起こる熱水循環の数値計算:日本海溝海側の高熱流量異常への応用Poster presentation
- Workshop on Ocean Mantle Dynamics: from Spreading Center to Subduction Zone, Oct. 2011, English, Chiba, Japan, International conferenceEstimation of 2-D resistivity structure beneath the Lau back-arc BasinPoster presentation
- Workshop on Ocean Mantle Dynamics: from Spreading Center to Subduction Zone, Oct. 2011, English, Chiba, Japan, International conferenceElectrical conductivity structure of the upper mantle beneath in the southern Mariana TroughPoster presentation
- Workshop on Ocean Mantle Dynamics: from Spreading Center to Subduction Zone, Oct. 2011, English, Chiba, Japan, International conferenceElectrical conductivity structure of a seafloor hydrothermal system at the southern Mariana Trough spreading axisPoster presentation
- Workshop on Ocean Mantle Dynamics: from Spreading Center to Subduction Zone, Oct. 2011, English, Chiba, Japan, International conferenceDevelopment of a 3-Dimensional Forward Program for Magnetometric Resistivity Method: Application to Alice Springs FieldPoster presentation
- Workshop on Ocean Mantle Dynamics: from Spreading Center to Subduction Zone, Oct. 2011, English, Chiba, Japan, International conferenceConstraint on a melting regime in upper mantle beneath the central Mariana back-arc spreading center through the geophysical electromagnetic forward modelingPoster presentation
- Workshop on Ocean Mantle Dynamics: from Spreading Center to Subduction Zone, Oct. 2011, English, Chiba, Japan, International conferenceComparison among available electrical resistivity structural images beneath back-arc and mid-ocean ridge spreading centersInvited oral presentation
- 東京大学地震研究所共同利用研究集会「沈み込み帯の温度構造と地震活動・変形過程」, Sep. 2011, Japanese, 東京大学地震研究所, 東京大学,東京, Domestic conference海洋プレートが沈み込む前後に起こる熱水循環はプレート内の温度分布をどう変えるか?Oral presentation
- 日本地球惑星科学連合2011年大会, May 2011, Japanese, 日本地球惑星科学連合, 幕張メッセ,千葉, Domestic conference南西インド洋中央海嶺35E-40E における地球物理観測から見る火成活動および断層活動のセグメント内での変化Oral presentation
- 日本地球惑星科学連合2011年大会, May 2011, Japanese, 日本地球惑星科学連合, 幕張メッセ,千葉, Domestic conference小笠原海台南東の北西太平洋海盆における地震波速度構造Oral presentation
- ブルーアース'11, Mar. 2011, Japanese, 東京, Domestic conference南マリアナトラフ背弧海盆拡大系における地球物理学的調査Oral presentation
- 東京大学地震研究所特定共同研究B研究集会「地球内部境界層の構造と全地球ダイナミクス」, Mar. 2011, Japanese, 東京, Domestic conference海底拡大系下の上部マントル比抵抗構造Oral presentation
- 2010年度CA研究会, Feb. 2011, Japanese, 京都, Domestic conferenceラウ背弧海盆拡大系における長期海底電磁場観測の概要Oral presentation
- 2010 AGU Fall meeting, Dec. 2010, English, USA, International conferenceThe MoHole: a Crustal Journey and Mantle QuestPoster presentation
- 海底拡大系の総合研究-InterRidge Japan研究発表集会-, Nov. 2010, Japanese, 千葉, Domestic conference地球物理観測に基づく南西インド洋海嶺東経35-40度における断層活動とメルト供給量に関する研究Oral presentation
- 海底拡大系の総合研究-InterRidge Japan研究発表集会-, Nov. 2010, Japanese, 千葉, Domestic conference海底拡大系の上部マントル比抵抗構造-これまでの研究と今後-Oral presentation
- 日本地質学会第117年学術大会, Sep. 2010, Japanese, 富山, Domestic conferenceモホールに向けて-掘削候補地の選定-Invited oral presentation
- 海洋技術創出シンポジウム, Jul. 2010, Japanese, 大阪, Domestic conference海底拡大系のダイナミクスOral presentation
- The International Workshop on The MoHole: A Crustal Journey and Mantle Quest, Jun. 2010, English, 金沢, International conferenceHawaii site in comparison with IODP site 1256Invited oral presentation
- 日本地球惑星科学連合2010年大会, May 2010, Japanese, 千葉, Domestic conference南西インド洋海嶺37°Eにおける上部マントル比抵抗構造の推定Oral presentation
- 日本地球惑星科学連合2010年大会, May 2010, Japanese, 千葉, Domestic conference南西インド洋海嶺34-40Eの超低速拡大セグメントの地球物理学的研究(KH0704-Leg2 and KH0905-Leg4)Oral presentation
- European Geoscience Union General Assembly 2010, May 2010, English, Austria, International conferenceMarine magnetotelluric survey across the Southwest Indian Ridge 37°EPoster presentation
- 2009年度CA研究会, Feb. 2010, Japanese, 東京, Domestic conference南西インド洋海嶺37°Eにおける上部マントル電気伝導度構造の推定Oral presentation
- 東京大学海洋研究所共同利用研究集会 海底拡大系の総合研究-InterRidge-Japan研究発表集会-, Oct. 2009, Japanese, 東京, Domestic conference南西インド洋海嶺、東経37度における電気伝導度構造探査Oral presentation
- 日本地震学会2009年秋季大会, Oct. 2009, Japanese, 京都, Domestic conferenceMohole 掘削に向けた地球物理学的研究 -戦略と計画-Oral presentation
- 地球電磁気・地球惑星圏学会第126回講演会, Sep. 2009, Japanese, 石川, Domestic conference北太平洋白亜紀海洋地殻の磁気異常-白亜紀スーパークロンの古地磁気強度変動の研究-Oral presentation
- 16th International Symposium on Polar Sciences, Jun. 2009, English, South Korea, International conferenceJapanese Marine Geophysical and Geological ResearchActivities in the Antarctic OceanPoster presentation
- 日本地球惑星科学連合2009年大会, May 2009, Japanese, 千葉, Domestic conference南西インド洋海嶺34°-40°Eに位置する斜交拡大海嶺の地球物理的研究Poster presentation
- 日本地球惑星科学連合2009年大会, May 2009, Japanese, 千葉, Domestic conference東南極大陸縁辺域リュツオ・ホルム湾沖での海底電磁気探査Oral presentation
- 日本地球惑星科学連合2009年大会, May 2009, Japanese, 千葉, Domestic conferenceTowing bipole electric current for marine magnetometric resistivity methodOral presentation
- CA研究会, Feb. 2009, Japanese, 京都, Domestic conference南極大陸縁辺域における海底下比抵抗構造探査Oral presentation
- Final SSP International Symposium on Deep Slab and Mantle Dynamics, Feb. 2009, English, 京都,日本, International conferenceElectrical structure in the mantle across the Mariana subduction systemPoster presentation
- 東京大学海洋研究所共同利用研究集会 海底拡大系の総合研究-InterRidge-Japan研究発表集会-, Oct. 2008, Japanese, 東京, Domestic conference海底地殻を冷却する『煙突』としての海山:数値実験による考察Oral presentation
- 東京大学海洋研究所共同利用研究集会 海底拡大系の総合研究-InterRidge-Japan研究発表集会-, Oct. 2008, Japanese, 東京, Domestic conferenceホットスポット影響下の南西インド洋海嶺(東経34 度‐40 度)における地球物理マッピング探査Oral presentation
- 東京大学海洋研究所共同利用研究集会 海底拡大系の総合研究-InterRidge-Japan研究発表集会-, Oct. 2008, Japanese, 東京, Domestic conferencePS 変換波を用いた海洋地殻内S 波速度構造の推定Oral presentation
- 第2回南極研究観測シンポジウム, Jun. 2008, Japanese, 東京, Domestic conference南極プレート周辺の海底拡大系の研究 その1:南東インド洋海嶺と南極-オーストラリア間のプレート運動の研究Oral presentation
- 日本地球惑星科学連合2008年大会, May 2008, Japanese, 千葉, Domestic conference北太平洋白亜紀海洋地殻の磁気異常―白亜紀スーパークロンにおける地球磁場強度変動の研究―Oral presentation
- 日本地球惑星科学連合2008年大会, May 2008, Japanese, 千葉, Domestic conference白鳳丸KH-07-4 Leg 2による南西インド海嶺34-40°E航海の概要Oral presentation
- 日本地球惑星科学連合2008年大会, May 2008, Japanese, 千葉, Domestic conference白鳳丸KH-07-4 Leg 2による南西インド海嶺34-40°E航海で採取された火山岩類の岩石学・地球化学Poster presentation
- 日本地球惑星科学連合2008年大会, May 2008, Japanese, 千葉, Domestic conference中部マリアナ沈み込み・前弧・島弧・背弧系の比抵抗構造Oral presentation
- 日本地球惑星科学連合2008年大会, May 2008, Japanese, 千葉, Domestic conference航空機重力異常から推定したゴンドワナ大陸の分裂に伴うリュツォ・ホルム湾周辺の大陸-海洋境界の地殻厚さ変化Oral presentation
- 日本地球惑星科学連合2008年大会, May 2008, Japanese, 千葉, Domestic conferencePS変換波を用いた海洋地殻内S波速度構造の推定Oral presentation
- 日本地球惑星科学連合2008年大会, May 2008, English, 千葉, Domestic conferencePreliminary report of surface geophysical survey at Southwest Indian Ridge 34-40E cruise (KH0704-Leg2)Poster presentation
- 第24回しんかいシンポジウム, Mar. 2008, Japanese, 横浜, Domestic conference沈み込み・前弧・島弧・背弧系(中部マリアナ海域)の電気伝導度構造Oral presentation
- 東京大学海洋研究所共同利用研究集会海洋リソスフェア学シンポジウム-海洋底深部構造と進化過程解明に向けて-, Mar. 2008, Japanese, 東京, Domestic conferenceマリアナ背弧拡大系の比抵抗構造-東太平洋中央海膨との比較-Oral presentation
- CA研究会, Dec. 2007, Japanese, 東京, Domestic conference中部マリアナ沈み込み・前弧・島弧・背弧系の電気伝導度構造Oral presentation
- Joint NSF-MARGINS and IFREE Workshop: Subduction Factory Studies in the Izu-Bonin-Mariana Arc System: Results and Future Plans, Nov. 2007, English, Hawaii, International conferenceMicroearthquake seismicity of the central Mariana Spreading CenterPoster presentation
- Joint NSF-MARGINS and IFREE Workshop: Subduction Factory Studies in the Izu-Bonin-Mariana Arc System: Results and Future Plans, Nov. 2007, English, Hawaii, International conferenceImaging mantle structure of the central Mariana subduction-arc-back arc system using marine magnetotelluricsInvited oral presentation
- Final SSP International Symposium on Deep Slab and Mantle Dynamics, Nov. 2007, English, 京都, International conferenceElectrical structure in the mantle across the Mariana subduction systemPoster presentation
- 特定領域研究「地球深部スラブ」第3回研究シンポジウム, Oct. 2007, Japanese, 松山, Domestic conference中部マリアナ沈み込み・前弧・島弧・背弧系の電気伝導度構造Poster presentation
- 海底拡大系の総合研究-InterRidge-Japan研究発表集会-, Oct. 2007, Japanese, 東京, Domestic conference中部マリアナ沈み込み・前弧・島弧・背弧系の電気伝導度構造Oral presentation
- 東京大学海洋研究所共同利用研究集会 海底拡大系の総合研究-InterRidge-Japan研究発表集会-, Oct. 2007, Japanese, 東京, Domestic conference中部マリアナ海域における海底地磁気変換関数Oral presentation
- 第27回極域地学シンポジウム, Oct. 2007, Japanese, 東京, Domestic conferenceゴンドワナの初期分裂時の東アフリカ沖モザンビーク海盆の海洋底拡大過程Oral presentation
- 地球電磁気・地球惑星圏学会第122回講演会, Sep. 2007, English, 名古屋, Domestic conferenceSeafloor GDS analysis in the central Mariana areaOral presentation
- 地球電磁気・地球惑星圏学会第122回講演会, Sep. 2007, English, 名古屋, Domestic conferenceMMR法による新潟沖メタンハイドレートの3次元イメージングOral presentation
- 南極研究観測シンポジウム, Jun. 2007, Japanese, 東京, Domestic conference南極プレート周辺の海底拡大系の研究Oral presentation
- 日本地球惑星科学連合2007年大会, May 2007, Japanese, 千葉, Domestic conference南インド洋東エンダビー海盆の地磁気異常Oral presentation
- 日本地球惑星科学連合2007年大会, May 2007, Japanese, 千葉, Domestic conference中部マリアナトラフ拡大軸付近の震源分布Oral presentation
- 日本地球惑星科学連合2007年大会, May 2007, Japanese, 千葉, Domestic conferenceゴンドワナの初期分裂時の東アフリカ沖モザンビーク海盆の海洋底拡大過程Oral presentation
- 日本地球惑星科学連合2007年大会, May 2007, English, 千葉, Domestic conferencePreliminary results of marine magnetotelluric analysis across the central Mariana transectOral presentation
- 日本地球惑星科学連合2007年大会, May 2007, Japanese, 千葉, Domestic conferenceMMR法による海底熱水循環系の3 次元比抵抗構造の推定Oral presentation
- CA研究会, Mar. 2007, Japanese, 京都, Domestic conference沈み込み・前弧・島弧・背弧系(中部マリアナ海域)の海底MT横断探査(序報)Oral presentation
- CA研究会, Mar. 2007, Japanese, 日本, Domestic conference沈み込み・前弧・島弧・ 背弧系(中部マリアナ海域)の海底MT横断探査(序報)Oral presentation
- 第23回しんかいシンポジウム, Mar. 2007, Japanese, 横浜, Domestic conference海底電位差磁力計による沈み込み・前弧・島弧・背弧系(中部マリアナ海域)の横断探査の概要Poster presentation
- 第 23 回しんかいシンポジウム, Mar. 2007, Japanese, 日本, Domestic conference海底電位差磁力計による沈み込 み・前弧・島弧・背弧系(中部マリアナ海域)の横断探査の概要Poster presentation
- CA研究会, Mar. 2007, Japanese, 日本, Domestic conferenceMMR 法の 3 次元フォワード解析手法と海底熱水循環系への応用Oral presentation
- CA研究会, Mar. 2007, Japanese, 京都, Domestic conferenceMMR法の3次元フォワード解析手法と海底熱水循環系への応用Oral presentation
- 東京大学海洋研究所共同利用研究集会中央海嶺研究のグローバルな展開-InterRidge-Japan研究発表集会-, Nov. 2006, Japanese, 東京, Domestic conference中部マリアナトラフ拡大軸上にある海底熱水循環系の3次元電気伝導度構造Oral presentation
- 東京大学海洋研究所共同利用研究集会中央海嶺研究のグローバルな展開-InterRidge-Japan 研究発表集会-, Nov. 2006, Japanese, 日本, Domestic conference中部マリアナトラフ拡大軸上にある海底熱水循環系の3次元電気 伝導度構造Oral presentation
- 東京大学海洋研究所共同利用研究集会中央海嶺研究のグローバルな展開-InterRidge-Japan研究発表集会-, Nov. 2006, Japanese, 東京, Domestic conference海底地震計より求めた中部マリアナトラフ拡大軸付近の震源分布Oral presentation
- 東京大学海洋研究所共同利用研究集会中央海嶺研究のグローバルな展開-InterRidge-Japan 研究発表集会-, Nov. 2006, Japanese, 日本, Domestic conference海底地震計より求めた中部マリアナトラフ拡大軸付近の震源分布Oral presentation
- 18th International Workshop on Electromagnetic Induction in the Earth El Vendrell - 2006, Sep. 2006, English, スペイン, International conferenceUndulation of 410-km discontinuity beneath the Philippine Sea plate as inferred from geomagnetic vertical gradient sounding method.Poster presentation
- 18th International Workshop on Electromagnetic Induction in the Earth El Vendrell - 2006, Sep. 2006, English, Spain, International conferenceUndulation of 410-km discontinuity beneath the Philippine Sea plate as inferred from geomagnetic vertical gradient sounding methodOral presentation
- 18th International Workshop on Electromagnetic Induction in the Earth El Vendrell - 2006, Sep. 2006, English, スペイン, International conferenceA newly developed three-dimensional forward program for the Magnetometric Resistivity method.Poster presentation
- 18th International Workshop on Electromagnetic Induction in the Earth El Vendrell - 2006, Sep. 2006, English, Spain, International conferenceA newly developed three-dimensional forward program for the Magnetometric Resistivity methodPoster presentation
- Ridge Theoretical Institute Meeting, Jun. 2006, English, アメリカ, International conferenceInvestigation of Sub-vent Biosphere through Aseptic Drilling into Arc and Backarc Volcanoes.Poster presentation
- Ridge Theoretical Institute Meeting, Jun. 2006, English, Mammoth Lakes, CA, USA, International conferenceInvestigation of Sub-vent Biosphere through Aseptic Drilling into Arc and Backarc VolcanoesPoster presentation
- 日本地球惑星科学連合2006年大会, May 2006, Japanese, 日本地球惑星科学連合, 幕張, Domestic conference日本海新潟沖ガスハイドレート域でのMMR法電磁探査Oral presentation
- 日本地球惑星科学連合2006年大会, May 2006, Japanese, 日本地球惑星科学連合, 幕張, Domestic conference地磁気鉛直勾配法で見たフィリピン海プレート下の410km不連続面Oral presentation
- 日本地球 惑星科学連合 2006 年大会, May 2006, Japanese, 日本, Domestic conference地磁気鉛直勾配法で見たフィリピン海プレート下の410km不連続面Oral presentation
- 日本地球惑星科学連合2006年大会, May 2006, Japanese, 日本地球惑星科学連合, 幕張, Domestic conference海底電気探査によるメタンハイドレートイメージングの試みOral presentation
- 日本地球惑星科学連合2006年大会, May 2006, Japanese, 日本地球惑星科学連合, 幕張, Domestic conference海底電位差磁力計による沈み込み・前弧・島弧・背弧系(中部マリアナ海域)の横断探査Oral presentation
- 日本地球 惑星科学連合 2006 年大会, May 2006, Japanese, 日本, Domestic conference海底電位差磁力計による沈み込み・前弧・島弧・背弧系(中部マリ アナ海域)の横断探査Oral presentation
- 日本地球惑星科学連合2006年大会, May 2006, Japanese, 日本地球惑星科学連合, 幕張, Domestic conferenceマリアナ背弧拡大系の地球物理学的研究[Invited]Invited oral presentation
- 日本地球惑星科学連合2006年大会, May 2006, Japanese, 日本地球惑星科学連合, 幕張, Domestic conferenceMMR法の磁場の3次元フォワード計算(その3)‐3次元フォワード計算から海底熱水循環系の3次元比抵抗構造を推定する‐Oral presentation
- 日本地球 惑星科学連合 2006 年大会, May 2006, Japanese, 日本, Domestic conferenceMMR 法の磁場の 3 次元フォワード計算(その 3)‐3 次元フォワー ド計算から海底熱水循環系の 3 次元比抵抗構造を推定する‐Oral presentation
- CA研究会, Dec. 2004, Japanese, 未記入, 東京, Domestic conference海底地形効果の補正についての検証Others
- CA研究会, Dec. 2004, Japanese, 未記入, 東京, Domestic conferenceメタンハイドレート検出を目指した海底電気探査装置の開発Others
- CA研究会, Dec. 2004, Japanese, 未記入, 東京, Domestic conferenceMagnetometric Resisticity Methodを用いた海底熱水循環系の電気伝導度構造の推定Others
- 2004 American Geophysical Union Fall Meeting, Dec. 2004, English, 未記入, San Francisco, USA, International conferenceHydrothermal circulation system in the central Mariana illustrated by Magnetometoric Resistivity experimentsPoster presentation
- 2004 American Geophysical Union Fall Meeting, Dec. 2004, English, 未記入, San Francisco, USA, International conferenceGeophysical features of hydrothermal system in Suiyo Seamount, Izu-Ogasawara Arc, Western PacificOthers
- 物理探査学会第111回学術講演会, Sep. 2004, Japanese, 物理探査学会, 岩手, Domestic conference自律型海中ロボットr2D4の深海地磁気三成分観測Others
- 物理探査学会第111回学術講演会, Sep. 2004, Japanese, 物理探査学会, 岩手, Domestic conferenceメタンハイドレード検出を目指した海底電気探査装置の開発Others
- 地球惑星関連学会2004年合同大会, May 2004, Japanese, 地球惑星関連学会, 幕張, Domestic conference水曜海山の地球物理学的構造と海底熱水循環系Others
- 地球惑星関連学会2004年合同大会, May 2004, Japanese, 地球惑星関連学会2, 幕張, Domestic conference初期コンドワナ分裂時の西エンダビー海盆の海底拡大Poster presentation
- 地球惑星関連学会2004年合同大会, May 2004, Japanese, 地球惑星関連学会, 幕張, Domestic conference重力異常から見たマリアナトラフ背弧拡大Poster presentation
- 地球惑星関連学会2004年合同大会, May 2004, Japanese, 地球惑星関連学会, 幕張, Domestic conference海底熱水循環系を電気伝導度で探るOthers
- 地球惑星関連学会2004年合同大会, May 2004, Japanese, 地球惑星関連学会, 幕張, Domestic conferenceマリアナ沈み込み帯上部マントルの電気伝導度構造(2) 次期高分解能観測のための数値シミュレーションPoster presentation
- 地球惑星関連学会2004年合同大会, May 2004, Japanese, 地球惑星関連学会, 幕張, Domestic conferenceマリアナ沈み込み帯上部マントルの電気伝導度構造(1) 2001-2002年海底MT観測の成果Others
- 地球惑星関連学会2004年合同大会, May 2004, Japanese, 地球惑星関連学会, 幕張, Domestic conferenceMMR制御電流を入力とした3次元電場・磁場の計算Poster presentation
- Ridge 2000-InterRidge Joint Theoretical Institute, Interactions among Physical, Chemical, Biological, and Geological Processes in Backarc Spreading Systems, May 2004, English, 未記入, Jeju Island, Korea, International conferenceAn overview on results of recent Japanese geophysical surveys in the Mariana areaPoster presentation
- アーキアン・パーク計画 平成15年度第2回課題検討会議, Jan. 2004, Japanese, 未記入, 山中湖, Domestic conferenceかいれい「KR03-13」Magnetometrc Resistivity Methodを用いた電気伝導度構造の推定Poster presentation
- アーキアン・パーク計画 平成15年度第2回課題検討会議, Jan. 2004, Japanese, 未記入, 山中湖, Domestic conferenceMMR制御電流を入力とした3次元電場・磁場の計算Poster presentation
- 地球惑星科学関連学会2003年合同大会, May 2003, Japanese, 地球惑星科学合同大会運営機構, 幕張, Domestic conference島弧の海底熱水系に特有な構造と性質と地下生物圏への影響Oral presentation
- 地球惑星科学関連学会2003年合同大会, May 2003, Japanese, 地球惑星科学合同大会運営機構, 幕張, Domestic conference中部マリアナ背弧系の電気伝導度構造Oral presentation
- 地球惑星科学関連学会2003年合同大会, May 2003, Japanese, 地球惑星科学合同大会運営機構, 幕張, Domestic conference中部マリアナトラフ拡大過程の復元Oral presentation
- 地球惑星科学関連学会2003年合同大会, May 2003, Japanese, 地球惑星科学合同大会運営機構, 幕張, Domestic conference瀬戸内海海底重力測定Oral presentation
- 地球惑星科学関連学会2003年合同大会, May 2003, Japanese, 地球惑星科学合同大会運営機構, 幕張, Domestic conferenceマリアナトラフの重力異常Oral presentation
- 地球惑星科学関連学会2003年合同大会, May 2003, Japanese, 地球惑星科学合同大会運営機構, 幕張, Domestic conferenceコントロールソースを用いた海底電磁気探査装置の開発(2)Oral presentation
- 地球惑星科学関連学会2003年合同大会, May 2003, Japanese, 地球惑星科学合同大会運営機構, 幕張, Domestic conferenceMMR法を道板中部マリアナトラフの拡大軸直下の電気伝導度構造の研究Oral presentation
■ Research Themes
- 日本学術振興会, 科学研究費助成事業, 基盤研究(A), 神戸大学, Apr. 2020 - Mar. 2024巨大カルデラ噴火を導いたマグマ供給系の現状把握研究目的を達成するために、鹿児島市の南約100kmの海域に位置する「鬼界海底カルデラ火山」を対象として、この巨大カルデラ火山のマグマ供給系全体の地球物理学的なイメージングを実施する。これにより、鬼界カルデラ直下に存在すると考えられる特徴的な構造の位置や大きさ等を把握する。 本年度は、巨大カルデラ火山のマグマ供給系全体のイメージングのために、現在実施している海底および陸上での地震観測と海底電磁気観測を継続するとともに、一部の観測機器の回収を行うことで観測データを取得した。まず、昨年度の3月に神戸大学の練習船「深江丸」の航海により回収した海底電位差磁力計(OBEM)を再設置するための準備として、必要な消耗品を購入と整備を行った。そして、7-8月に実施されたJAMSTECの海底広域研究船「かいめい」のKM21-05航海により、昨年度設置した短周期海底地震計(SPOBS)と海底磁力計(OBM)の回収およびOBEMの再設置を行った。また、10月に実施した練習船「深江丸」の航海においても、SPOBSの回収を行った。さらに、昨年度に広帯域地震計を設置した臨時陸上観測点で、観測機器の点検と観測データの回収と、一部の地点で磁力計の設置も行い、観測はそのまま継続している。 得られた観測データの解析を順次進めている。まず、OBEMにより得られた海底電磁場変動データからMTレスポンスを求め、1次元の比抵抗構造を推定した。一方で、海底で得られたMTレスポンス等をもちいて3次元比抵抗構造を推定するためのインバージョン手法の開発を進めた。また、SPOBSおよび陸上観測で得られた地震波形データから、観測網の直下で発生していた地震のデータを取り出し、走時を用いたローカルトモグラフィ解析の準備を進めた。 翌年度に計画している海底観測機器の回収のために航海申請等を行い、この航海に必要な準備を始めた。
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for Scientific Research (A), Apr. 2020 - Mar. 2023Development of AI for autonomous ship handling to accelerate ocean-bottom exploration, and its demonstration at actual sea本研究では,気象海象が複雑に変化する状況下において,海洋底探査に課せられた高度ミッションを達成するための自律操船AIの開発を行っている。今年度の研究実績の概要は以下の通り。 ①深層強化学習により,海洋調査に用いられる測線トラッキング用の自律操船AIの開発を行った。風,波,潮流が混在する中での直線航路のトラッキングに加えて,測線の終了点から次の測線の始点を直線で繋いだ不連続な航路に対しても最小の偏差で追従可能とするために,測線と自船の位置関係をニューラルネットワークへの入力としている。開発したAIの評価のため,水産研究・教育機構の漁業調査船「たか丸」を使用して,AIの舵角指示をディスプレイに表示し,船員(人間)がそれに応じて操舵する半自動操船システムを構築した。そのうえで,複数回の実船実験を通じて,船内情報収集システムの検証やAIのトラッキング精度について検証を行った。本システムはAIの判断を効果的に伝達するインターフェースが重要であるため,複数の船員に操船してもらい改善すべき事項についてフィードバックコメントを収集した。 ②風,波,潮流という外乱作用下での定点保持操船の自動化のために、舵角だけでなく,CPPのプロペラ翼角とバウスラスターのオンオフを行動に含めたプロトタイプのAIを開発し,「たか丸」で検証実験を実施した。 ③水産技術研究所の海洋工学総合実験棟において,次年度に実施を予定しているAIによる定点保持操船の模型実験に向けた予備的実験を行った。
- 科学研究費補助金/基盤研究(B), Apr. 2015 - Mar. 2019, Principal investigatorCompetitive research funding
- 科学研究費補助金/基盤研究(B), Apr. 2015 - Mar. 2019, Principal investigatorCompetitive research funding
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for Scientific Research on Innovative Areas (Research in a proposed research area), The University of Tokyo, Apr. 2008 - Mar. 2014Geological and geophysical background of subseafloor hydrothermal systems "TAIGA"The integrated geological and geophysical field surveys were conducted on the hypothesis that the diversity of subsealoor hydrothermal circulation (TAIGA: Great River) is controlled by tectonic and geological setting beneath and around the hydrothermal fields. The series of AUV and submersible dives and geophysical explorations showed that the sulfur-rich hydrothermal sites in the southern Mariana backarc spreading center are controlled mainly by the waxing and waning of magmatic activity. In contrast, the results of geological, geophysical surveys and rock geochemistry revealed that the hydrogen-rich Kairei hydrothermal field at the southernmost Central Indian Ridge is constrained by both axial basaltic magmatism and detachment faulting that exhume ultramafic rocks on a shallow subsurface.
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for Scientific Research (A), Kobe University, 2009 - 2011, Principal investigatorInvestigations on melt region structures beneath spreading axes are a key to understand back-arc spreading system. We developed a compact ocean bottom magnetometer(OBM), which was designed to be attached to US ocean bottom seismograph(OBS); that became first ocean bottom seismograph and magnetometer(OBSM) in the world achieved by an international cooperation. We carried out one year ocean bottom observation near the Eastern Lau spreading axis using the instruments. Marine magnetotelluric analysis using ocean bottom data allows us to image the resistivity structures of the upper mantle beneath the spreading axis, which were compared to identify differences in melt region structures and to understand the cause of the differences.Competitive research funding
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for Scientific Research (B), The University of Tokyo, 2007 - 2009Does mantle geochemistry control the mid-ocean ridge process?-Southwest Indian Ridge expeditionThe geophysical and geochemical survey was done along the ultraslow spreading Southwest Indian Ridge 31-41°E. Geophysical data shows the spatial and temporal variation of the melt supply in the area, which corresponds to the variation of mid-ocean ridge process such as spreading asymmetry and obliquity. The result of rock analysis also suggests the existence of small-scale heterogeneity of mantel geochemistry and/or temperature. The upper mantle structure and microseismicity are also revealed.
- 日本学術振興会, 科学研究費補助金/特定領域研究, 特定領域研究, 神戸大学, 2005 - 2006, Principal investigator前年度に調べた電気伝導度構造、地震波速度構造の2つの違った構造と沈み込み帯の上部マントルでの物性量の関係から、それぞれの構造と物性量の関係が比較的明らかな異方性に注目した.地震学的観測データによるS波速度の異方性は、各観測点におけるS波スプリッティングで生じた、速いS波の振動方向と、速いS波と遅いS波の時間差によって調べられるため、異方性が生じている深度の情報が含まれていない.一方、電磁気的観測データでは、異方性の方向とその程度の分解能は低いが、深度に関する情報が含まれている.このため、S波スプリッティングの結果を使い、上部マントル物質であるオリビンの異方性に関する物性から条件をつけて、電磁気的観測データを解析する手法の検討を行った.さらに、これによる電気伝導度異方性構造を推定する解析手法の開発を現在も進めている. 研究協力者である大学院生(岩本)を同じく研究協力者であるワシントン大学のDouglas A.Wiens教授に派遣して地震学的観測データの解析を行った.マリアナ背弧海盆拡大軸付近の海底地震計による観測データを解析することにより、この付近で起こる微少な地震の震源分布を明らかにした.また、Wiens教授のグループの大学院生であるS.H.Pozgayが、同じ海底地震計による地震観測データを解析することにより、各観測点におけるS波スプリッティングを調べ、速いS波の振動方向と速いS波と遅いS波の時間差の空間分布を明らかにしつつあった.この結果を、開発中の電気伝導度異方性構造を推定する方法に、どのように適用するかにっいての検討も行った.現実のデータにおいては、S波の振動方向や時間差には、空間的なばらつきがあるため、直接に組み込むことができず、単純化する必要があることがわかった.Competitive research funding
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for Scientific Research (B), Kobe University, 2005 - 2006, Principal investigatorWe carried out a marine magnetotelluric transect across the central Mariana subduction-arc-back arc system using ocean bottom electro-magnetometers (OBEMs), ocean bottom electrometers (OBEs), and ocean bottom magnetometers (OBMs) to provide the electrical conductivity structure of the Mariana island-arc system extending from the Pacific ocean to the West Mariana Ridge (remnant arc) through the Marina Trough. Deployments of 33 OBEMs, 7 OBMs, and 7 OBEs were made at 40 sites across the central Mariana subduction-arc-back arc system during KR05-17 cruise. Observations using the instruments were made from December 2005 up to the recovery in September 2006. We successfully recovered 28 OBEMs, 7 OBMs, and 6 OBEs at 35 sites during KR06-12 cruise. We are still analyzing these data to estimate the upper mantle electrical conductivity structure, because the observation was delayed. But, these data will provide a comprehensive image of the conductivity structure for the central Mariana subduction-arc-back arc system, because the observation sites are so dense. We analyzed previous 9 OBEM data obtained from the same area. The resulting electrical resistivity structure shows an increase in conductivity at depths of about 70 km beneath the Mariana Trough and anisotropy at deeper depth. The low conductivity structure near Mariana Trough spreading axis implies that the onset of melting in the Mariana Trough back-arc basin is deeper than that of the typical MORB source region. Consideration of the effect of seafloor topography on ocean bottom magnetotelluric data is needed to estimate a reliable conductivity structure. We evaluated three different correction equations to correct the effect of seafloor topography with forward modeling, and we indicate the most an appropriate correction method based on a series of synthetic tests.Competitive research funding
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for Scientific Research (B), Nagoya University, 2004 - 2006Exploration of sub-seafloor methanehydrate using artificial current source ocean-bottom electromagnetic method and its reservoir estimation1. A deep-towed electrical sounding system was developed for shallow ocean-bottom conductivity survey, especially for precise determination of the upper limit of hydrate layers. A sensitivity analysis was done in term of the parameters such as the depth, thickness and concentration of the hydrate layer using a electrical-field response modeling code. Optimum design of the observation system was investigated. 2. Improvement of the artificial current source and the Ocean-Bottom ElectroMagnetic equipment (OBEM) was done in Kobe University. JAMSTEC developed smaller-size OBEMs. 3. EM modeling and inversion codes were developed. Discontinuity in the conductivity structure was introduced in the 2-D inversion code, enabling to image sharp layer structures and faults. A 3-D magnetometric modeling code was developed to calculate anomalous magnetic field caused by any 3-D resistivity structure. 4. In the first cruise (Off Sado, August 2005), the newly developed deep-towed electrical sounding system was tested at the depth of 1000 meters below sea-surface and successfully obtained electrical potential data. The electrical resistivity structure from 0 to about 100 meters below sea-floor was analyzed. It was proved that the resistivity structure was consistent to the visual inspection of the sea floor. The distribution of the hydrate was in columnar shape and was first imaged. MMR method using the artificial current source and the OBEMs revealed a low amplitude anomaly of magnetic field in the west of the survey area, suggesting the localized existence of the resistive hydrate in the area. In the second cruise (Off Tokai, February 2006), the operation of the deep-towed electrical system was again in success. The resistivity structure from 0 to about 100 meters below sea-floor was in good agreement with the result of the resistivity logging in the test drilling done in 1999. The two field test proved the reliability and effectiveness of the developed deep-towed electrical sounding system.
- 2006惑星系の起源と進化Competitive research funding
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for Scientific Research (A), The University of Tokyo, 2002 - 2005Integrated Research on the Mid-oceanic Ridge by Internationally Co-operated ExpeditionsThis project promoted InterRidge Japan as a part of InterRidge International Project with the financial supports for the payment of member's fee of InterRidge (20,000-25,000 US$ annually), travels of Japanese ridge scientists for participating domestic and international mid-oceanic ridge research cruises and InterRidge meetings such as an InterRidge steering committee, InterRidge Symposiums, Workshops, and Theoretical Institutes, and for inviting foreign ridge research scientists. By these supports Japan made a principal contribution to the InterRidge (current number of the member countries is 29) as one of five principal member countries with UK, US, France, and Germany. Two members of this projects are appointed as members of the InterRidge Steering Committee. During four years, 14 mid-oceanic research cruises were conducted with the partial financial supports by this project. The research fields cover marine geology, marine geophysics, water geochemistry, marine biology, and ocean technology. Japan specially contributed in the fields of hydrothermal geochemistry, marine microbiology, and ocean technology. AUV (Autonomous Underwater Vehicle) expedition with three-component magnetometer installed demonstrated the demagnetization of the crust according to the extent of hydrothermal activity at the Mariana Trough in the Western Pacific. Regional water circulation in the oceanic crusts around the mid-oceanic ridge was evidenced by IODP Juan de Fuca Ridge drilling for which this project made partial financial support. The cooperated expedition research at the Southwestern Indian Ridge found wide exposures of mantle rocks on the sea floor which suggest a fundamental mechanism of ultra-slow spreading system with very low magmatism. In 2006 diving research cruises were conducted at the hydrothermal area at the Central Indian Ridge and we succeeded to obtain valuable samples of microbiology and hydrothermal mineralization which analyses are currently ongoing.
- 2005惑星系の起源と進化Competitive research funding
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for Scientific Research (B), Kobe University, 2001 - 2002Conductivity structure around seismogenic layer beneath the Chugoku and Shikoku districtsWe delineated the Philippine Sea plate beneath the South-western Japan arc using the electro-magnetic method in this study. The Network-MT method is one of the magnetotelluric methods and it is suitable for surveying a conductivity structure beneath a wide area and to a deep portion. We applied the method in Chugoku and Shikoku district to reveal a subsurface structure beneath the South-west Japan arc. We focused on the where and how does the Philippine Sea Plate exist. The first reason is that a location of The Philippine Sea plate is most important factor to controlled occurrences of earthquakes, because the cold and rigid plate makes large influence on a thermal state and/or a distribution of seismic-wave velocity. Second reason is that it is hard to decide a location of the plate using only seismic methods. The precise 2-dimensional conductivity model was established. This model is characterized by following points. 1) North dipping resistive layer (> 500Ω・m) exists beneath both Chugoku and Shikoku districts. The upper depth of the resistive layer is 20km, 30km beneath the southern and northern part of the Shikoku district, and 40km, 60km beneath the southern and northern part of the Chugoku district, respectively. 2) Conductive layer (~100Ω・m) exists beneath the north dipping resistive layer. 3) Highly conductive layer is found at 40km-depth beneath the northern most part of the Chugoku district. We interpreted the north dipping resistive layer is the Philippine Sea plate.
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for Scientific Research (B), Kobe University, 2000 - 2002Spreading process of the Mariana TroughThe Mariana Trough is a typical intra-oceanic back-arc basin that shows a variety of features. We have compiled extensive surface geophysical data (bathymetry, magnetic and gravity) of the Mariana Trough, which were collected during several Japanese cruises over the last few years. Topographic features and the mantle Bouguer anomaly (MBA) reveal distinct differences between regions. The north of 22N shows extremely low MBA indicating an incipient rifting. The central region between 21N and 14N shows characteristic slow-spreading features; existence of median valley neovolcanic zone and "Bull's eyes" MBA along the axes. The south of 14N shows an EPR type axial relief morphology and lower MBA than that in the central. Tectonic evolution can be inferred from the direction of spreading fabric, the trace of non-transform offsets, and by crustal ages identified by vector geomagnetic anomaly field. The crustal ages indicate that the seafloor spreading started at 4Ma, 6Ma and 3Ma at the northern end, the central, and the southern end, respectively. The spreading rates are generally slow (~20 mm/yr) in the northern and central areas, while they are fast (~35 mm/yr) in the south. Spreading axis directions have gradually changed by 15 degrees clockwise with age in the north of 17.5N, while they occurred at 3.5-3.0Ma from N35W to N5W just south of 17.5N. On the other hand, they are relatively constant in the southern end. We have developed a new type of ocean bottom electro-magnetometer (OBEM), which is small and easy to handle with Filloux-type electrodes. Preliminary results of an OBEM observation for one year in the Mariana region suggest that very conductive zone (about 70km in depth) below the Marianas island arc and low conductivity zone with thickness of a few ten km beneath the Mariana Trough.
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for Scientific Research (A), The University of Tokyo, 1999 - 2001International Cooperative Research on the mid-Oceanic Ridges-Earth Environmental Dynamics and Mid-Oceanic RidgeThis budget is the Japanese counterpart of the InterRidge program. The budget is used for travels of the Japanese scientists and transportation of the instruments for research cruises, travels of the Japanese scientists to participate InterRidge meetings, and travels for invited foreign scientists. 1. Results of mid-oceanic ridge research cruises The Japanese scientist members of this project participated 12 research cruises in the Western Pacific, Indian Ocean, Northern Atlantic, and the back-arc basins. The research fields cover tectonics, geochemistry, seismology, petrology, biology and microbiology. Major achievements are the discover of the first active vent site in the Indian Ocean, identification of hotspot-ridge interaction at the Aden rift system in the Indian Ocean., and mapping of segment configuration of the Knipovich Ridge in the Arctic Sea. 2. Promotion of InterRidge program The Japanese scientist members of this project intensively participated steering committees, workshops, symposiums, and theoretical institutes organized by InterRidge. As the activity of the Japanese scientists for InterRidge project, the steering committee approved to move the InterRidge Office to Japan for 4 years from 2000. The Office is now at the Ocean Research Institute, and K. Tamaki serves as a chairman. 3. Invitation of foreign scientists We invited a number of scientists from Russia, England, Yemen, and France to do the summary discussion of the research cruises and to devise future program plan. Two new proposals for the mid-oceanic ridge of the Atlantic ocean were submitted through the discussion with the invited foreign scientists.
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for international Scientific Research, Chiba University, 1996 - 1998Structure and Tectonics of Japan Sea and Sikhote Alin and their relation to Japan Arcl.Research in the Japan Basin During this cooperative research, the marine investigations had been carried out by R/V Prof.Gagarinsky of POI on the tracks of 5 mile interval in the whole area of Japan Basin in the Russian EEZ.. a.Seismic investigation : OBSs of Chiba University and the single air-gun of P01 were used for the seismic research in the Japan Basin resulting in that the thickness of crust in the central part of the Japan Basin is 8-9km including 1.5km thick sediments and increasing towards east. The feature of crust is not completely identical with the typical oceanic one.The crust in the eastern part of the Basin is oceanic, then the central part of the Basin has the different developing mode from the east part, namely sea floor spreading development. b.Magnetic investigation : A proton precession magnetometer of POI and a STCM(Shipboard Three Component Magnetomete) of Chiba Univ. were used for the magnetic study of the Basin resulting in that there are clear magnetic anomaly lineations in the eastern part of the Basin and not so clearly in the cental part. This is coincident with the seismic investigation mentioned above. c.Gravity investigation : A shipboard gravimeter of POI was used. The structures of the crust obtained from gravity anomalies change from the oceanic to the continental from east to west. 2.Research in the Sikhote Alin (Geological Research) The geological investigation was done to reconstruct the original position of Japanese islands before opening of the Japan Sea using the geological data in the SikhoteAlin especially of Tercialy time. The geological continuation between the Japanese islands and the Sikhote Alin in the Tercially time was revealed taking other data, that are, tobography of the Basin floor and deformation of the Japanese Island Arc into account.
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for international Scientific Research, the University of Tokyo, 1996 - 1998International Cooperative Research on the mid-Oceanic RidgesThis program corresponds to the InterRidge program, an international initiative of mid-oceanic ridge studies. The funds of this program are mainly used for travels of ridge researchers in Japan for participating cruises, attending workshops, program planning meetings, and society meetings. The other part of usage is transportation of instruments for the research cruises. The research cruises that the researchers of this program participated cover the global ridge system including the Juan de Fuca Ridge, the East Pacific Rise, the Mid-Atlantic Ridge, the Southwestern Indian Ridge, the Central Indian Ridge, and the western Pacific back-arc basins ridges. The major achievements were done in the studies in the Southwestern Ridge. Five research cruises were executed at the Southwestern Indian Ridge during this program. Multinarrow bathymetric survey, deep-tow sidescan sonnar survey, gravity and magnetic measurements, ocean bottom seismometer measurements, and bottom rock sampling were done. The compilation of these data sets clearly shows the unique segmentation pattern of this ridge, the ultraslow spreading system with striking heterogeneity of crustal structure and intensively focused magmatism.
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for international Scientific Research, The University of Tokyo, 1995 - 1997Electromagnetic and Tomographic Research of Melt below EPRAs for geophysical measurements around the East Pacific Rise (EPR four Ocean Bottom Electro Magnetometers (OBEMs) were successfully retrieved during a research cruise from the end of May/'97 through the beginning of July/'97 by R/V Melville of Scripps Institution of Oceangraphy, US,to yield electromagnetic (EM) time series at the seafloor for more than one year. The OBEMs have been installed at 17゚S of EPR during a previous research cruise from the middle of May/'96 through the beginning of July/'96, which was also an international cruise coordinated by Mantle ELectromagnetic and Tomography (MELT) Project. The EM data from these seafloor units are now being analyzed together with those simultaneously collected by US and Australian groups. The goal of the analyzes and subsequent modellings/inversions is reveal the EM structure of melt bodies just below the super spreading center. Specifically, this research aims at quantifying the geometry, melt fraction and connectedness of the melt bodies by a joint observation of seismics and magnetotellurics at the seafloor. In terms of study of the very old oceanic crust in Archaen, rock sampling was conducted in South Africa and Zimbabwe this year. The samples collected are either igneous or sedimentary rocks as old as 2,500 to 3,500 Ma. These samples are in the course of petrological, geological and paleomagnetic analyzes to yield estimates of the tectonic activity at the seafloor and Earth's geomagnetic field in Archaen, which will be combined with the results from the samples collected in Australia ('95) and in Canada ('96) to give reconstruction of a worldwide view of the Earth in Archaen.
- 日本学術振興会, 科学研究費助成事業, 一般研究(B), 東京大学, 1995 - 1995高感度マグネットテルリック法で中央海嶺下溶融体の底を見る「海底電磁気データから中央海嶺下溶融体の深部構造を決定する方法を確立」する事を主眼に本年度の研究を進めた。本研究では、(1)磁場データの感度向上、(2)長周期(具体的には潮汐周期帯)信号の開拓、(3)電磁場のmigrationに基づいた構造解析法(イメージング法)の導入、の3点からこの目的を達成する事を試みた。(1)により、電場に比べ明らかに感度が足りない事が分かって来た磁場データを高感度で採取する事で厚い海水のスクリーニングを受けても浅部構造を精密に決める事が可能になる。(2)では、新しい時系列解析法を開発し海洋潮汐により海洋中でキネマティックに誘導される電磁場を信号源として活用する事により、上部マントルの持つコンダクタンスの上限値が制約条件として得られ、(1)で得られた浅部構造と組み合わせる事によって、中央海嶺下部に存在する溶融体の「底」が見えて来る。また(3)では、時間領域及び周波数領域における電磁場のmigrationに基づいたイメージング法を新たに導入し、これを従来の電気伝導度構造解析と組み合わせる事により、海底電磁気データの形状決定に対する分解能の向上につながる。 (1)の測器改良では、高感度3成分磁場センサーを導入する事により磁場感度の向上を実現でき、改良した測器を伊豆小笠原弧をテストフィールドとした海域実験に投入し高感度磁場データを取得する事が出来た。(2)の海洋潮汐を信号源とする新しい解析法、及び、(3)の電磁場のmigrationを利用した新しい構造解析法、についても必要なソフトウェア群は一応の完成をみた。但し、海域実験の時期が本年度後半にずれ込んだ為、観測データの一部はまだ解析の途上にあり実測データに基づく新しい解析手法の有効を検証するまでには至っていない。しかしながら、ほぼ所期の目的を達成する事が出来たと考えられる。