| Project/Area Number |
12480147
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| Research Category |
Grant-in-Aid for Scientific Research (B)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
Environmental dynamic analysis
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| Research Institution | The University of Tokyo |
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Principal Investigator |
MATSUMOTO Ryo GRADUATE SCHOOL OF SCIENCE, PROFESSOR, 大学院・理学系研究科, 教授 (40011762)
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| Co-Investigator(Kenkyū-buntansha) |
TOKUYAMA Eiichi OCEAN RESEARCH INSTITUTE, PROFESSOR, 海洋研究所, 教授 (10107451)
OGIHARA Shigenori GRADUATE SCHOOL OF SCIENCE, RESEARCH ASSOCIATE, 大学院・理学系研究科, 助手 (50214044)
TADA Ryuuji GRADUATE SCHOOL OF SCIENCE, PROFESSOR, 大学院・理学系研究科, 教授 (30143366)
HIROKI Yoshihisa OSAKA KYOUIKU UNIVERSITY, ASSOCIATE PROFESSOR, 教育学部, 助教授 (80273746)
ASHI Juichiro OCEAN RESEARCH INSTITUTE, ASSOCIATE PROFESSOR, 海洋研究所, 助教授 (40251409)
木下 正高 東海大学, 海洋学部, 助教授 (50225009)
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| Project Period (FY) |
2000 – 2002
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| Project Status |
Completed (Fiscal Year 2002)
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| Budget Amount *help |
¥14,600,000 (Direct Cost: ¥14,600,000)
Fiscal Year 2002: ¥700,000 (Direct Cost: ¥700,000)
Fiscal Year 2001: ¥3,700,000 (Direct Cost: ¥3,700,000)
Fiscal Year 2000: ¥10,200,000 (Direct Cost: ¥10,200,000)
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| Keywords | Nankai Trough / DBSR / ODPLeg204 / Cascadia margin / Kuroshima Knoll / Methane seep / Carbonate nodules / Dolomite / ガスハイドレート / 塩分濃度 / 酸素同位体組成 / 永久凍士 / 塩素濃度 / 水素同位体組成 / ヨウ素 |
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| Research Abstract |
1. Double BSR was reported from the eastern Nankai Trough in 1995. This research has conducted extensive analysis of seismic profiles obtained by JNOC methane hydrate project, and has revealed that DBSRs are widely distributed in the eastern Nankai Trough. This implies that this unique phenomena were probably caused by regional geologic events.
2. Submersible dives to the area where DBSR were recognized were not so productive during the cruise. However, carbonate nodules which were incidentally collected from the northern extension of DBSR area by fisherman showed very interesting data, indicating that the area experienced strong methane expultion, and strong methane flux were caused by gas hydrate dissociation.
3. Variable types of carbonate nodules were collected from active methane seep sites on the Kuroshima Knoll off Ishigaki Island. Geochemical signatures of the nodules indicate that chimney like nodules are all composed of dolomite, carbonate carbon is strongly depleted in 13C and enriched in 18O, suggesting influence of methane and hydrate-derived waters.
4. Large number of water and sediment samples have been collected from the Cascadia margin off Vancouver, Canada, where DBSRs are identified below active methane seep sites. Geochemical analysis has revealed that top sediments are characterized by positive anomaly of chloride, seep gases contain significant amount of thermogenic methane, and sulfate concentration of pore waters decrease with depth depending of methane flux.
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