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Oral presentation

Distribution and feature of the fracture zones of active faults

Niwa, Masakazu

no journal, , 

no abstracts in English

Oral presentation

Current status of the geoscientific research for long-term stability of the geological environment in the JAEA R&D programme

Umeda, Koji; Nohara, Tsuyoshi; Yasue, Kenichi

no journal, , 

no abstracts in English

Oral presentation

Current status and plan of MIU project

Iwatsuki, Teruki

no journal, , 

We summarize the results and plan on Phase 1 and 2 of MIU project. The methodology to estimate the basesline condition prior to construction of MIU facility was demonstrated. Based on such research, the plan on study and engineering development in Phase 2 of project were presented.

Oral presentation

Oral presentation

Study of variation in mechanical properties of Toki granite

Hashiba, Kimihiro

no journal, , 

no abstracts in English

Oral presentation

Investigation of earthquake related groundwater level changes at the MIU Construction Site

Salden, W.; Takeuchi, Shinji; Takeuchi, Ryuji; Saegusa, Hiromitsu

no journal, , 

no abstracts in English

Oral presentation

Outline of research for engineering technology at Mizunami Underground Research Laboratory

Sato, Toshinori; Kuji, Masayoshi

no journal, , 

no abstracts in English

Oral presentation

About the summary of post grouting test of ground around shaft

Hara, Masato

no journal, , 

no abstracts in English

Oral presentation

Development of research technique for the activity of magma and high-temperature fluid in the deeper part beneath the Japan arcs

Ninomiya, Atsushi

no journal, , 

Geothermal activity is originated from magma or hot rock beneath the Quaternary volcanoes. High-temperature hot springs distribute around Iide Mountains showing high heat discharge values although the area is a nonvolcanic region of the Northeast Japan Arc. In this study, Iide Mountains were imaged by wide-band magnetotelluric soundings. A two-dimensional model shows that anomalous conductive body is clearly visible beneath the Iide Mountains. The location of the conductive body correlates with high-temperature hot springs of high $$^{3}$$He/$$^{4}$$He ratio. The temperature of the conductive body is estimated as above 400 $$^{circ}$$C on the basis of thinning of the brittle seismogenic layer. We conclude that the conductor reflects the presence of partial melts in the crust, related to renewed magmatism in the present-day subdction system.

Oral presentation

History of the geoscientific studies in the Tono Mine after the H12 report

Sasao, Eiji

no journal, , 

no abstracts in English

Oral presentation

Oral presentation

Oral presentation

Overview of the regional hydrogeological study

Saegusa, Hiromitsu; Iwatsuki, Teruki; Amano, Kenji; Tsuruta, Tadahiko; Takeuchi, Ryuji; Seno, Yasuhiro; Matsuoka, Toshiyuki; Mizuno, Takashi

no journal, , 

no abstracts in English

Oral presentation

Development of ACROSS (Accurately Controlled Routinely Operated Signal System) as a next-generation precise geophysical exploration method

Kunitomo, Takahiro; Nakajima, Takahiro; Hasada, Yoko*; Fujii, Naoyuki; Kumazawa, Mineo

no journal, , 

no abstracts in English

18 (Records 1-18 displayed on this page)
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