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MATSUNO TetsuoOcean-Bottom Exploration Center (KOBEC)Associate Professor
Research activity information
■ Paper- Elsevier BV, Sep. 2025, Journal of Volcanology and Geothermal Research, 465, 108369 - 108369[Refereed]Scientific journal
- Understanding the distribution of physical properties around shallow subducting plate interfaces, where both destructive and "slow" earthquakes occur due to rapid and slower fault slips, respectively, presents a major scientific and disaster mitigation challenge. Pore water is a key factor in understanding the different slip mechanisms and their spatial relationships; however, its distribution remains understudied. In this study, based on marine magnetotelluric survey in Hyuga-nada, southwestern Japan, we identified distinct resistive and conductive anomalies along the plate interface. These anomalies correspond to areas of scarce pore fluid and high concentration area of pore fluids sourced from subducting seamounts (Kyushu-Palau Ridge), respectively. The wet area corresponds to the slow slip area, whereas the dry and transition areas correspond to areas of fast fault slip. These findings provide clear observational evidence that pore fluid distribution correlates with fault rupture behavior.May 2025, Scientific reports, 15(1) (1), 17077 - 17077, English, International magazine[Refereed]Scientific journal
- The Volcanological Society of Japan, Dec. 2024, BULLETIN OF THE VOLCANOLOGICAL SOCIETY OF JAPAN, 69(4) (4), 223 - 228, Japanese[Refereed]
- 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
- The Volcanological Society of Japan, 2024, PROGRAMME AND ABSTRACTS THE VOLCANOLOGICAL SOCIETY OF JAPAN, 2024, 217 - 217, Japanese
- Mar. 2022, JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 127(3) (3), e2021JB022374, English[Refereed]Scientific journal
- Kikai Caldera volcano has repeatedly erupted in large scale eruptions such as the Kikai Akahoya eruption 7,300 years ago and the Kikai Tozurahara eruption 95,000 years ago, and detailed eruption history can be studied by combining seafloor and on-land surveys.In this study, core samples were collected by the SCORE program of CHIKYU based on the subsurface structure revealed by seismic reflection surveys of large eruptive ejecta on the seafloor, which are still largely unknown.The chemical composition of the volcanic glass was analyzed and compared with subaerial deposits, and it was found that the two large-scale eruptive ejecta are thickly deposited on the seafloor as well, and that the Kikai Akahoya product is divided into two units on the seafloor as well.In addition, the chemical compositional characteristics of volcanic glass in piston core samples from a wide area around the Kikai caldera suggest that the Kikai Akahoya product may have become less accessible to distant sites as the eruption progressed.GEOCHEMICAL SOCIETY OF JAPAN, 2022, Abstracts of Annual Meeting of the Geochemical Society of Japan, 69, 95, Japanese
- Sep. 2020, Geophysical Journal International, 222(3) (3), 1502 - 1525, English[Refereed]Scientific journal
- Aug. 2019, Tectonophysics, 768, 228182, English[Refereed]Scientific journal
- Jul. 2018, Earth, Planets and Space, 70(1) (1), 111 - 111, English[Refereed]Scientific journal
- Feb. 2018, Scientific Reports (Nature Publishing Group), 8(1) (1), 2753 - 2753, English, International magazine[Refereed]Scientific journal
- Oct. 2017, EARTH PLANETS AND SPACE, 69(1) (1), 138 - 138, English[Refereed]Scientific journal
- Aug. 2017, EARTH PLANETS AND SPACE, 69(1) (1), 111 - 111, English[Refereed]Scientific journal
- Lead, Mar. 2017, EARTH AND PLANETARY SCIENCE LETTERS, 462, 189 - 198, English[Refereed]Scientific journal
- Lead, Jun. 2015, POLAR SCIENCE, 9(2) (2), 221 - 234, English[Refereed]Scientific journal
- Lead, Springer Japan, Jan. 2015, Subseafloor Biosphere Linked to Hydrothermal Systems: TAIGA Concept, 241 - 251, English[Refereed]In book
- Mar. 2014, GEOPHYSICAL JOURNAL INTERNATIONAL, 196(3) (3), 1365 - 1374, English[Refereed]Scientific journal
- Oct. 2012, EARTH AND PLANETARY SCIENCE LETTERS, 351, 45 - 53, English[Refereed]Scientific journal
- Oct. 2012, GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 13(10) (10), Q10017, English[Refereed]Scientific journal
- Lead, Sep. 2010, GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 11(9) (9), Q09003, English[Refereed]Scientific journal
- Jun. 2007, PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 162(1-2) (1-2), 2 - 12, English[Refereed]Scientific journal
- Lead, 2007, EARTH PLANETS AND SPACE, 59(8) (8), 981 - 986, English[Refereed]Scientific journal
- 2006, 不明, 38741, EnglishOn Board Cruise Report of KR06-12 Kairei CruiseScientific journal
- 2003, JAMSTEC Journal of Deep Sea Research, 22, 22, 89-106 - 106Preliminary report of KR02-14 Kairei cruise
- Nov. 2024, 地球電磁気・地球惑星圏学会総会及び講演会(Web), 156thStudy of Tide-Induced Electromagnetic Field Response in the Kikai Caldera Sea Area
- Sep. 2024, The 26th Electromagnetic Induction Workshop (EMIW2024)3-D resistivity modeling based on marine magnetotelluric data in the Kumano-nada, southwestern Japan arc
- Sep. 2024, The 26th Electromagnetic Induction Workshop (EMIW2024)Electrical resistivity modeling in megathrust earthquake regions of hot and cold subduction margins along Japan Island Arc
- Sep. 2024, The 26th Electromagnetic Induction Workshop (EMIW2024)Estimation of 3-D resistivity structure under the Kikai submarine caldera volcano
- The Volcanological Society of Japan, Sep. 2024, 日本火山学会講演予稿集, 2024, 49 - 49, Japanese
- The Volcanological Society of Japan, Sep. 2024, 日本火山学会講演予稿集, 2024, 218 - 218, Japanese
- Conductivity Anomaly Research Group, Jul. 2024, Proceedings of the Conductivity Anomaly Workshop, 2024, 18 - 20, Japanese
- May 2024, 日本地球惑星科学連合大会予稿集(Web) 2024 2024年 2024年5月熊野灘における海底電磁場観測と海底地形を考慮した三次元比抵抗モデリング
- May 2024, 日本地球惑星科学連合大会予稿集(Web) 2024 2024年 2024年5月3-D resistivity structure under the Kikai submarine caldera volcano
- May 2024, 日本地球惑星科学連合大会予稿集(Web) 2024 2024年 2024年5月最終氷期以降における大阪湾の音響層序と地殻変動
- May 2024, 日本地球惑星科学連合大会予稿集(Web) 2024 2024年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
- Mar. 2024, 海と地球のシンポジウム発表課題一覧・要旨集(CD-ROM), 2023鬼界カルデラ火山海域での地下比抵抗構造
- 大阪湾は、上町断層帯や六甲・淡路島断層帯、中央構造線断層帯など、いくつかの主要活断層帯によって囲まれた閉鎖性海域である。六甲・淡路島断層帯においては1995年に兵庫県南部地震(気象庁マグニチュード7.3)が発生しており、2013年にも気象庁マグニチュード6.3の地震が淡路島で発生している。また、大阪府北部においては、2018年に気象庁マグニチュード5.5の地震が発生している。これまでの反射法地震探査の結果から、大阪湾断層帯と呼ばれる北東-南西走向で約39 km延びている北西側隆起の逆断層帯が大阪湾西部で確認されており、このような大規模な断層だけでなく、他にも数多くの活断層が発達している(岩淵ほか, 1995)。大阪湾内全域の断層分布や活動履歴を把握することは、大阪湾にかかる応力とそれによるテクトニックな変遷を理解するために重要である。また、海底下に存在する断層は津波を引き起こす可能性もあるため(たとえば河田ほか, 2005)、大阪湾付近にある大都市の災害のリスク評価にも役立てることができる。 本研究では、大阪湾において、最終氷期以降(約18,000年前以降)の断層活動の影響を受けていると考えられる沖積層の層厚分布を面的に作成すること、および、小断層を見つけ、その分布や活動履歴を把握することを目的とした。解析に用いたデータは、2022年8月、10月、および2023年3月に神戸大学の練習船「海神丸」に搭載されたKongsberg社のサブボトムプロファイラーTOPAS PS18によって大阪湾中・南部を対象として1~3 km間隔の格子状に広範囲に取得した。一般的な反射法地震探査で用いる音源は100 Hz程度の低周波であるのに対して、サブボトムプロファイラーは1-10 kHz程度の高周波であるため、反射法地震探査と比べて、高分解能のデータを得ることができる。本調査では、帯域幅2~6 kHz、信号長1 msのチャープ波を主に使用した。調査の結果、底下30 m程度の沖積層や洪積層上部に関して数十cm程度の細かい層を認定できるような高分解能のデータが得られた。 データ解析では、まず音響基盤となる洪積層より上位の沖積層を地震学的に3~5の堆積ユニットに区分した。OpendTectやPetrelを用いて海底面や各堆積ユニットの境界面をピックし、QGISを用いて、境界面の深度の差を取ることから各堆積ユニットの層厚分布を面的に得ることができ、各堆積ユニットの深度変化をマッピングすることができた。区分した堆積ユニットの年代の制約には過去に行われたボーリング調査の結果(たとえば七山ほか, 2000)を用いた。断面上で断層を確認した位置もマッピングを行った。大阪湾断層帯以外の顕著な変形構造として、岩淵ほか(2000)で津名沖断層として記載されている活断層の近傍に撓曲構造を確認した。この撓曲構造は表層付近まで変位が確認できることから、最近まで活動していたことが考えられ、今後活動履歴を詳細に考察する必要がある。本発表では、これらの堆積ユニットの層厚分布を面的に示して、大阪湾における過去の海底面や堆積環境の復元や断層活動との関連を議論する予定である。引用文献:岩淵ほか(1995)大阪湾西部の活断層, 海洋調査技術, 7, 11-19岩淵ほか(2000)反射法音波探査に基づく大阪湾の基盤と活構造, 水路部研究報告, 36, 1-23河田ほか(2005)大阪湾臨海都市域の津波脆弱性と防災対策効果の評価, 海岸工学論文集, 52, 1276-1280七山ほか(2000)大阪湾断層及び和田岬断層の完新世活動性調査, 平成11年度活断層・古地震研究調査概要報告書, 179-193The Geological Society of Japan, 2023, Annual Meeting of the Geological Society of Japan, 2023, 226, Japanese
- 2023, 海と地球のシンポジウム発表課題一覧・要旨集(CD-ROM), 2022鬼界カルデラ破局噴火のマグマ準備過程
- 2023, 海と地球のシンポジウム発表課題一覧・要旨集(CD-ROM), 2022鬼界海底カルデラの総合調査
- 2023, 海と地球のシンポジウム発表課題一覧・要旨集(CD-ROM), 2022鬼界カルデラ火山海底下の三次元比抵抗構造解析
- 2023, 海と地球のシンポジウム発表課題一覧・要旨集(CD-ROM), 2022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
- 2023, 日本地球惑星科学連合大会予稿集(Web), 2023Low-velocity anomaly beneath Kikai-caldera submarine volcano, Japan, revealed by seismic refraction survey
- 2023, 日本地球惑星科学連合大会予稿集(Web), 2023Investigation of extraction method of high-quality electromagnetic data for marine MT survey
- The Volcanological Society of Japan, 2023, 日本火山学会講演予稿集, 2023 (Web), 147 - 147, Japanese
- 2023, 地球電磁気・地球惑星圏学会総会及び講演会(Web), 154thImaging a 3-D resistivity structure under the Kikai submarine caldera volcano.
- 2023, 日本地質学会学術大会(Web), 130thThe distribution of small faults and acoustic stratigraphy of the alluvium in the Osaka Bay, Japan, revealed by sub-bottom profiler data
- [東京] : CA研究グループ, 2022, Conductivity anomaly研究会論文集, 47 - 51, JapaneseOBEMおよびNetwork-MTデータの統合解析による日向灘周辺の3次元比抵抗構造の推定—Three-dimensional resistivity modeling around the Hyuga-nada area based on OBEM and Network-MT data
- 2022, 地球電磁気・地球惑星圏学会総会及び講演会(Web), 152ndDevelopment of 3D resistivity structure analysis method considering the effects of seafloor topography.
- 2022, 日本地球惑星科学連合大会予稿集(Web), 2022Late Pleistocene to Holocene dynamic basin environment at the Osaka Bay: Stratigraphic expressions of tectonic deformation, sea level fluctuation, and tidal waves
- 2022, 日本地球惑星科学連合大会予稿集(Web), 2022Amphibious passive seismic observation at Kikai submarine caldera
- The Volcanological Society of Japan, 2022, PROGRAMME AND ABSTRACTS THE VOLCANOLOGICAL SOCIETY OF JAPAN, 2022, 70 - 70, Japanese
- Kikai submarine caldera caused several catastrophic eruptions. In order to understand the eruption processes and magmatic evolution, we measured chemical composition of tephra collected via the SCORE program with D/V Chikyu. We used submarine tephra from the K-Ah eruption (7300 years ago), that from the K-Tz eruption (95000 years ago), and that intercalated between the two catastrophic eruptions, the age of which is approximately 40000 years ago or younger. The tephra from the K-Tz eruption is predominated by felsic pyroclasts, but the presence of a few mafic pyroclasts suggests the contribution of mafic melts during the K-Tz eruption. The tephra intercalated between the two catastrophic eruptions have chemical composition similar to those of K-Ah, implying that the storage of felsic magmas commenced at least 40000 years ago toward the next catastrophic eruption of K-Ah.GEOCHEMICAL SOCIETY OF JAPAN, 2022, Abstracts of Annual Meeting of the Geochemical Society of Japan, 69, 96, Japanese
- 2021, 日本地球惑星科学連合大会予稿集(Web), 2021Development of a 3D inversion code to consider ocean bottom magnetotelluric data including topographic distortion~forward modeling part~
- 2021, 日本地球惑星科学連合大会予稿集(Web), 2021Sedimentary structures caused by submarine landslide southern Satsuma Peninsula
- 2021, 日本地球惑星科学連合大会予稿集(Web), 2021Bathymetric Survey and Tsunami Modeling of a Submarine Landslide in Tosa-bae, Nankai trough
- 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
- 東京 : 物理探査学会, 2021, 物理探査学会学術講演会講演論文集, 144th, 68 - 71, Japanese3-D resistivity analysis around the Hyuga-nada area based on marine-MT data
- The Volcanological Society of Japan, 2021, 日本火山学会講演予稿集, 2021, 75 - 75, Japanese
- 2021, 海と地球のシンポジウム発表課題一覧・要旨集(CD-ROM), 2021海底の鬼界アカホヤ噴火堆積物の特徴
- 2021, 海と地球のシンポジウム発表課題一覧・要旨集(CD-ROM), 2021鬼界海底カルデラにおける物質科学的研究の現状
- In April 2013, the Japanese Government settled on the second stage of an oceanic basic plan that emphasized the development of ocean resources and the enhancement of oceanic education. In light of this situation, KOBEC (Kobe Ocean-Bottom Exploration Center) was established at Kobe University on October 1, 2015. Afterwards, preparations for ocean-bottom exploration activities using the training ship Fukae-maru were advanced by KOBEC. KOBEC will develop various promotion programs for its activities, for instance, the development of exploitation technology of ocean-bottom resources and specially-designed exploration techniques, etc. centering on the advanced research of the ocean bottom. In the Review of Graduate School of Maritime Sciences, Kobe University No.14 (June, 2017), the actual situation of the early exploration activities in addition to sufficiency of the deployment and the equipment for new observation apparatus for ocean bottom exploration activities was investigated in detail. The routine exploration activities around Kikai Caldera and the accumulation of observation data recently progressed into full operations. The exploration activities and detailed report of ship services of the first six voyages after starting acquisition and accumulation of observation data are summarized in this paper. This report aims to be helpful in further developing exploration activities sequentially in the future. In addition, the progress of the further results of research and instructional activities of KOBEC challenges is considered.神戸大学大学院海事科学研究科, 2020, 神戸大学大学院海事科学研究科紀要, 17, 1 - 23, Japanese
- 2020, 日本地球惑星科学連合大会予稿集(Web), 2020Short to long term morphological changes and migration of sand waves in a semi-enclosed sea: a case study in Okinose area of Osaka Bay
- 2020, 日本地球惑星科学連合大会予稿集(Web), 2020Structure of submarine mass-transport complexes(MTCs) southern Mt.Kaimon
- 2020, 日本地球惑星科学連合大会予稿集(Web), 2020Estimation of MT response function to reveal resistivity structure around the Hyuganada area
- 2020, 地球電磁気・地球惑星圏学会総会及び講演会(Web), 148th3-D resistivity modeling around the Hyuganada area
- 2020, 海と地球のシンポジウム発表課題一覧・要旨集(CD-ROM), 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
- 2020, 海と地球のシンポジウム発表課題一覧・要旨集(CD-ROM), 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-
- The Volcanological Society of Japan, 2019, PROGRAMME AND ABSTRACTS THE VOLCANOLOGICAL SOCIETY OF JAPAN, 2019, 51 - 51, Japanese
- 2019, 日本地球惑星科学連合大会予稿集(Web), 2019海底MTアレイデータを用いた海洋上部マントルの一次元異方性電気伝導度構造の推定
- 2019, 日本地球惑星科学連合大会予稿集(Web), 2019四国沖大陸棚斜面の海底地すべり調査と津波計算
- 2019, 日本地球惑星科学連合大会予稿集(Web), 2019開聞岳南方海域の崩れ地形の成因を海底地形とマルチチャンネル反射波地震探査から探る
- 2019, 日本地球惑星科学連合大会予稿集(Web), 2019火山ガラス組成に基づく鬼界カルデラ海底採取火山灰と幸屋火砕流堆積物の対比
- 2019, 日本地球惑星科学連合大会予稿集(Web), 2019大阪湾の海底に見られるサンドウェーブの移動
- 2019, 日本地球惑星科学連合大会予稿集(Web), 2019ROVによる鬼界カルデラ海底調査の予察的報告
- 2019, 歴史地震(Web), (34) (34)徳島県宍喰沖海底地すべり痕のマルチナロービーム測深
- 2019, 日本地球惑星科学連合大会予稿集(Web), 2019Summary of Kikai submarine caldera researches conducted by KOBEC (Kobe Ocean-Bottom Exploration Center)
- 2019, 日本地球惑星科学連合大会予稿集(Web), 2019鬼界カルデラのMT観測データの解析
- 2019, 日本地球惑星科学連合大会予稿集(Web), 2019鬼界カルデラ下の3次元電気比抵抗構造探査
- 2018, 日本地震学会秋季大会講演予稿集(CD-ROM), 2018四国沖大陸棚斜面の海底地すべりの地形調査
- 2018, 地球電磁気・地球惑星圏学会総会及び講演会(Web), 144th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
- 2018, 日本地球惑星科学連合大会予稿集(Web), 2018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
- 2018, 日本地球惑星科学連合大会予稿集(Web), 2018The characteristics of seismic stratigraphic facies of Kikai submarine caldera and off the southern Kyusyu
- 2018, 日本地球惑星科学連合大会予稿集(Web), 2018Integrated marine investigations of Kikai Caldera, SW Japan
- 2017, Earth and Planetary Science Letters, 462Mantle transition zone beneath a normal seafloor in the northwestern Pacific: Electrical conductivity, seismic thickness, and water content
- 2016, Conductivity Anomaly研究会論文集, 2016Mantle transition zone beneath a normal seafloor in the northwestern Pacific: Electrical conductivity, seismic discontinuity, and water content
- 2016, 日本地球惑星科学連合大会予稿集(Web), 2016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
- 2016, 日本地球惑星科学連合大会予稿集(Web), 2016Mantle transition zone beneath a normal seafloor in the northwestern Pacific: Electrical conductivity, seismic discontinuity, and water content
- 2015, 日本地球惑星科学連合大会予稿集(Web), 2015「ふつう」の海洋マントルの電気伝導度構造イメージング
- 2015, 日本地球惑星科学連合大会予稿集(Web), 2015「ふつうの海洋マントル」プロジェクトにおけるマントル遷移層電気伝導度構造の解明
- 2015, 日本地震学会秋季大会講演予稿集, 2015海底電磁気・地震同時観測データから推定する北西太平洋「ふつう」の海洋マントル遷移層の含水量
- 2014, ブルーアース要旨集, 2014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
- 2011, 地球電磁気・地球惑星圏学会総会及び講演会予稿集(CD-ROM), 130th多目的関数最適化アルゴリズムにもとづくMT一次元異方性比抵抗構造インバージョン
- 2011, 地球電磁気・地球惑星圏学会総会及び講演会予稿集(CD-ROM), 130th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
- 2011, ブルーアース要旨集, 2011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
- 2011, 地球電磁気・地球惑星圏学会総会及び講演会予稿集(CD-ROM), 130thラウ背弧海盆下の2次元比抵抗構造の推定
- Mar. 2008, しんかいシンポジウム予稿集, 24th, 38, Japanese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
- 2006, しんかいシンポジウム予稿集, 22nd日本海新潟沖におけるメタンハイドレート域総合調査
- Jan. 2003, しんかいシンポジウム予稿集, 19th, 126 - 127, Japaneseマリアナ諸島周辺のマントルウェッジ電気伝導度構造
- 日本地球惑星科学連合2019年大会, May 2019, Japanese海底MTアレイデータを用いた海洋上部マントルの一次元異方性電気伝導度構造の推定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 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
- 日本地震学会2018年度秋季大会, Oct. 2018, Japanese, ビッグパレットふくしま(福島県郡山市), Domestic conference四国沖大陸棚斜面の海底地すべりの地形調査Oral presentation
- 日本歴史地震研究会, Sep. 2018, Japanese, Oita City, Domestic conference徳島県宍喰沖海底地すべり痕のマルチナロービーム測深Oral 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
- 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
- IAG-IASPEI symposium 2017, Aug. 2017, English, International conferenceMantle transition zone beneath a normal seafloor in the northwestern Pacific: Electrical conductivity, seismic discontinuity, and water contentOral presentation
- IAG-IASPEI symposium 2017, Aug. 2017, English, International conferenceEstimation of electrical anisotropy in the oceanic upper mantle from seafloor magnetotelluric array dataPoster presentation
- IAG-IASPEI symposium 2017, Aug. 2017, English, International conferenceConstraints on lithospheric mantle and crustal anisotropy in the NoMelt area from an analysis of long-period seafloor magnetotelluric dataPoster presentation
- JpGU-AGU Joint Meeting 2017, May 2017, English, 幕張メッセ, International conferenceSimple plate cooling model is no longer applicable to the upper mantle beneath the northwestern Pacific: Evidence from marine magnetotelluricsOral 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 conferenceEstimation of electrical anisotropy in the oceanic upper mantle from seafloor magnetotelluric array dataPoster 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
- 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
- Japan Geoscience Union Meeting 2016, May 2016, English, International conferenceMantle transition zone beneath a normal seafloor in the northwestern Pacific: Electrical conductivity, seismic discontinuity, and water contentOral 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
- 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
- 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
- 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 conferenceConstraint on a melting regime in upper mantle beneath the central Mariana back-arc spreading center through the geophysical electromagnetic forward modelingPoster presentation
■ Research Themes
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for Scientific Research (A), The University of Tokyo, 01 Apr. 2023 - 31 Mar. 2027International collaborative research on the viscosity of the oceanic asthenosphere through marine geophysical observations and geodynamic modeling
- 日本学術振興会, 科学研究費助成事業 基盤研究(A), 基盤研究(A), 神戸大学, 01 Apr. 2020 - 31 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、海底および陸上での地震観測と海底電磁気観測を開始した。 ・観測に必要な機器である、広帯域海底地震計(BBOBS)、短周期海底地震計(SPOBS)、海底磁力計(OBM)、海底電位差磁力計(OBEM)、陸上用の広帯域地震計の準備を行った。BBOBS、SPOBS、OBEMについては、電池、切り離し部品を含む錘などの必要な消耗品を購入し、海底に設置するための整備を行った。OBMをSPOBSに取り付けるための治具の作成やその準備を行った。また、OBMの専用データロガーを4台購入して台数を増やした。一方、陸上用の広帯域地震計は、1セット分を購入するともに、必要な消耗品を購入して既存の分の整備も行った。 ・9月~10月に実施されたJAMSTECの深海調査研究船「かいれい」のKR20-11航海に必要な準備を行った。この航海により「鬼界海底カルデラ火山」とその周辺海域の海底に、BBOBS、SPOBS、OBM、OBEMの設置を行い、海底での観測を開始した。 ・臨時陸上観測点は、鬼界カルデラに近い三島村、および水深上の制約で海底地震計の設置が難しい鬼界カルデラ東方をカバーするために種子島と屋久島に、広帯域地震計を設置し、陸上での地震観測を開始した。 ・2月~3月に実施された神戸大学の練習船「深江丸」の航海により、8台のOBEMを回収した。回収したOBEMにより得られた海底電磁場変動データを確認し、その観測データの解析を開始した。
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (C), Grant-in-Aid for Scientific Research (C), The University of Tokyo, 01 Apr. 2015 - 31 Mar. 2019This study aims to investigate the distribution of water in the mantle transition zone beneath the western Pacific region using the seafloor electromagnetic observation data collected by our research group in the last decade. For this purpose, we focused on the natural magnetic field variations in the period range that the data is sensitive to the depth of the mantle transition zone, and attempted to develop new analysis methods; 1) separating the complex magnetic field components from the observed data, and 2) incorporating the complex spacial distribution of the magnetic field which is used for the inversion analysis to image the electrical conductivity in the mantle transition zone.
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (B), Grant-in-Aid for Scientific Research (B), Kobe University, Apr. 2015 - Mar. 2019Our main results of 2-D electrical resistivity structure and of numerical simulation lead us to propose a hypothesis that the low viscosity region in the mantle wedge due to hydration driven by water release from the subducting slab results in highly asymmetric seafloor spreading, which is commonly recognized in many back-arc basins. The resistivity structure was imaged through marine magnetotelluric experiment across a spreading segment in the Southern Mariana Trough back-arc basin. This result shows that a low resistivity region exists beneath the spreading axis and is asymmetrically extended to the subducting slab; the low resistivity region is interpreted as asymmetric melting in the mantle wedge due to hydration driven by water release from the subducting slab. Further, numerical simulation results indicate that the spreading axis is kept locating above the low viscosity mantle zone that capture the mantle upwelling zone due to water release from the subducting slab.
- Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (A), Grant-in-Aid for Scientific Research (A), Kobe University, 2009 - 2011Investigations 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.