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Interdisciplinary and international cooperative studies on fluid circulations in the Nankai Trough accretionary prism

Interdisciplinary and international cooperative studies on fluid circulations in the Nankai Trough accretionary prism
南海海槽吸积棱体流体循环的跨学科国际合作研究
批准号:
06044042
负责人:
GAMO Toshitaka
金额:
$9.73万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for international Scientific Research
财政年份:
1994
资助国家:
日本
项目状态:
已结题
起止时间:
1994 至 1996

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中文摘要
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英文摘要
The purpose of this project is to promote interdisciplinary studies on fluid circulation, crustal deformation and biological activities in the Nankai Trough accretionary prism, as part of the Japan-France cooperative KAIKO-TOKAI Project. Since the beginning of the KAIKO project in 1984, it has been known that the northwestward subduction of the Philippine Sea plate under the Eurasian plate forms a huge accretionary prism along the Nankai Trough, where circulating fluid in sedimentary layrs, accompanied with cold seepage on the sea bottom, likely plays an important role in causing large-scale crustal deformation such as big earthquakes. The KAIKO-TOKAI Project aims at elucidating geophysical, geological, geochemical and ecological characteristics of the accretionary prism, by using research vessels and submersibles. During 1994-1996,3 cruises of R/V Hakuho Maru (Ocean Research Institute, University of Tokyo), 2 cruises of R/V Tansei Maru (Ocean Research Institute, University of Tokyo), 1 cruise of R/V L'Atalante (IFREMER,France), 12 dives of DSRV Shinkai 2000 (JAMSTEC) and 8 dives of DSRV Shinkai 6500 (JAMSTEC) were devoted for this project. Results obtained during these cruises and dives have been presented and discussed at the KAIKO-TOKAI Steering Committee meetings, which were held in Japan and France once in each year. Remarkable results so far obtained are as follows : (i) another subduction was identified along the southern rim of the Zenisu Ridge by OBS observations and differential GPS measurements, (ii) Detailed crustal structure has been revealed by 120 channel seismic surveys, (iii) H_2S production by sulfate reduction (methane oxidation) was first confirmed through isotope measurements of methane dissolved in pore fluids from accretionary prism sediment, etc. The KAIKO-TOKAI project will last till the end of the 1997 fiscal year, when an international symposium will be held in Japan in order to review this project totally.
期刊论文(111)
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科研奖励(0)
会议论文
S.Nakashima: "Diffusivity of ions in pore water as a quantitative basis for rock deformation rate estimates" Tectonophysics. 245. 185-203 (1995)
S.Nakashima:“孔隙水中离子的扩散率作为岩石变形率估计的定量基础”构造物理学。
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通讯作者:
M.Kinoshita and M.Yamano: "Heat flow distribution in the Nankai Trough Region ---Geology and Geophysics of the Philippine Sea Floor" In : Geology and Geophysics of the Philippine Sea (ed by H.Tokuyama et al.),Terra Scientific Publishing Company,Tokyo. 77-
M.Kinoshita 和 M.Yamano:“南海海槽地区的热流分布 --- 菲律宾海底的地质学和地球物理学”,载于:菲律宾海的地质学和地球物理学(由 H.Tokuyama 等编辑),Terra
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小泉金一郎ほか: "瀬戸内海における海上重力測定" 測地学会誌. 40. 333-345 (1994)
Kinichiro Koizumi 等人:“濑户内海的海洋重力测量”大地测量学会杂志 40. 333-345 (1994)。
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通讯作者:
P.Henry et al.: "Fluid expulsion in and around a mud volcano field seaward of the Barbados accretionary wedge:results of the "Manon" cruise" Journal of Geophysical Research. (in press).
P.Henry 等人:“巴巴多斯增生楔向海的泥火山场及其周围的流体排出:“曼农”号巡航的结果”地球物理研究杂志。
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89
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