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Goto, Akira; Murakami, Masaki*; Sakai, Ryutaro*; Terusawa, Shuji*; Sueoka, Shigeru
JAEA-Review 2020-003, 60 Pages, 2020/03
One of the natural phenomena that may affect the geological disposal system are earthquake and fault activity. Fault displacement due to the earthquake and fault activity will be considered the direct effects. In addition to it, it is necessary to consider the secondary effects include secondary faults formed by the seismic fault activity as well as spring water and mud volcanoes that are generated by fluid movement attributed to the fault activity. This paper introduces previous studies performed focused on the hydraulic effects (spring water and mud volcanoes) and mechanical effects (secondary faults) in order to understand the effects of these secondary phenomena on the geological disposal system. We were able to collect 142 literatures from Japan and overseas by searching for related keywords in Japanese and English. As a result, we compiled case studies of each secondary impact. From the viewpoint of geological disposal, we extracted the following issues for future research and development. As for the sump water induced by earthquakes and faulting, accumulation of information related to its mechanism, affected area, and activity history is required. As for the mud volcanoes, reviewing of the mechanism of anomalous pore water pressure that causing the formation, also development of estimation technique are required. And for the secondary faults, accumulation of the detailed spatial distribution and reviewing of formation mechanism are required.
Sueoka, Shigeru; Ikuho, Zuitetsu*; Hasebe, Noriko*; Murakami, Masaki*; Yamada, Ryuji*; Tamura, Akihiro*; Arai, Shoji*; Tagami, Takahiro*
Journal of Asian Earth Sciences; X (Internet), 2, p.100011_1 - 100011_11, 2019/11
no abstracts in English
Yamada, Kunimi; Murakami, Masaki*; Tagami, Takahiro*; Yamada, Ryuji*
no journal, ,
no abstracts in English
Yamada, Kunimi; Murakami, Masaki*; Tagami, Takahiro*; Yamada, Ryuji*
no journal, ,
We indicate a relation between heating conditions and helium retentions using zircons heated under ultra short term and hydrothermal conditions. It is important that samples heated in less than one minutes for fault samples. Because the durations of hydrothermal heating are from 10 to 100 hours constrained by technical limitations, the effects of water and pressure are examined through comparison with same durations of dry heating.