Fluid distribution around a seismogenic zone along a plate boundary fault imaged and monitored by controlled source electromagnetic sounding
Fluid distribution around a seismogenic zone along a plate boundary fault imaged and monitored by controlled source electromagnetic sounding
批准号:
17340134
负责人:
GOTO Tada-nori
金额:
$8.74万
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (B)
财政年份:
2005
资助国家:
日本
项目状态:
已结题
起止时间:
2005 至 2007
中文摘要
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英文摘要
In FY 2005, we carried out three feasibility studies and tests for long term monitoring of seimogenic zone. A numerical calculation codes for marine controlled source electromagnetic survey was developed. Marine DC resistivity surveys were conducted at two research cruises. Seismic records of aftershocks of the Sumatra great earthquakes were analyzed. These studies are helpful for new development and refinement of cabled long-term ocean bottom electromagnetometers and ocean bottom seismometers. In FY 2006, underwater tests for these ocean bottom instruments were carried out in a small pool. Also, the off-Toyohashi cable, located on the Tokai mega-earthquake zone, was pulled up by using a cable ship and was deployed after attaching a junction unit to the end. In FY 2007, the newly developed ocean bottom instruments were connected to the junction unit at the end of off Toyohashi cable. The JAMSTEC vessels and a ROV were used for the seafloor operations. As a result, a multidisciplinary c … More abled observatory, whose targets are submarine earthquakes, crustal deformation and groundwater flow below the seafloor, was constructed off-Toyohashi, just on the Tokai mega-earthquake zone. Continuous artificial electric signals are sent from the off-Toyohashi cable simultaneously, so that the first ocean bottom monitoring of electrical conductivity variation below the seafloor was started.Before the continuous seafloor monitoring, marine magnetotelluric surveys were carried out off-Toyohashi area to image the crustal electrical conductivity structure around the Tokai mega-earthquake zone. Twelve instruments were deployed and recovered successfully. The obtained data set show us the conductivity structure of subducting Philippine Sea plate.As a result, several papers and presentations were presented through this project, relating to the cabled observatory, marine controlled source electromagnetic survey and electromagnetic phenomena possibly excited by groundwater flow below the seafloor. Less
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通信用光海底ケーブルを再利用した豊橋沖観測システムの概要
重复利用海底光缆进行通信的丰桥近海观测系统概述
DOI:
--
发表时间:
2007
期刊:
月刊地球 29
影响因子:
--
作者:
[Kasaya, T., 後藤忠徳, 浅川賢一]
通讯作者:
浅川賢一
Crustal resistivity structure around the Nankai subduction zone(Reviewed)
南开俯冲带周围地壳电阻率结构(综述)
DOI:
--
发表时间:
2005
期刊:
Butsuri-tansa(Geophysical Exploration) 58
影响因子:
--
作者:
[Kimura, T]
通讯作者:
T
DOI:
--
发表时间:
2005
期刊:
影响因子:
--
作者:
[Goto, T.]
通讯作者:
T.
DOI:
10.1186/bf03353367
发表时间:
2006-01-01
期刊:
EARTH PLANETS AND SPACE
影响因子:
3
作者:
[Araki, E, Shinohara, M, Suyehiro, K]
通讯作者:
Suyehiro, K
Outline of the off-Toyohashi seafloor observation system utilizing a decommissioned underwater optical telecommunication cable
利用退役水下光通信电缆的丰桥外海底观测系统概要
DOI:
--
发表时间:
2007
期刊:
Chikyu Monthly 29
影响因子:
--
作者:
[Asakawa, K]
通讯作者:
K
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