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Oral presentation

Study for self-sealing process of EDZ and flow-paths factures learnt from spherical carbonate concretion formation

Yoshida, Hidekazu*; Yamamoto, Koshi*; Maruyama, Ippei*; Karukaya, Koichi*; Nakayama, Masashi; Sakurai, Akitaka; Sato, Toshinori

no journal, , 

Spherical, isolated carbonate concretions occur throughout the world in marine argillaceous sedimentary rocks of widely varying geological ages. These concretions are characteristically highly enriched in CaCO$$_{3}$$ compared to the surrounding sedimentary rock matrices and are commonly containing the well-preserved fossils inside. Recently the process of the enrichment of CaCO$$_{3}$$ has been revealed and synthetic concretion materials are developed. Here we will introduce the in-situ experiment with the synthetic concretion material for EDZ sealing carried out in Horonobe Underground Research Laboratory and the preliminary results of the EDZ sealing process and their sealing effectiveness.

Oral presentation

Examination of modeling of Quaternary volcanic central conduit and radial dikes by topographic analysis using GIS software

Nishiyama, Nariaki*; Kawamura, Makoto; Umeda, Koji*; Goto, Akira; Niwa, Masakazu

no journal, , 

The authors assume that the topography of the mountain body reflects the actual distribution area of the dike, and we are developing a method to do the model the distribution area of the center conduit and radial dikes by topographical analysis of the mountain body using GIS software. In this study, we proposed a method that enables topographical analysis volcanoes whose activity history is not clear, conducted topographical analysis at each volcano, and modeled the distribution area of dikes. As a result, the analysis method used in this study made it possible to capture the features of the topography formed by the activity of the volcano without including the expert judgement. This makes it possible to compare the analysis results of this study with the geology, and this analysis results are considered to be useful information. In addition, the distribution tendency of the centroid of each altitude obtained in this study shows the results consistent with the wide-area stress field at the time of the eruption, and shows the validity of the analysis results.

Oral presentation

Estimation of in-situ formation factor in fractured rocks using resistivity from laboratory experiment

Murakami, Hiroaki; Fukuda, Kenji*; Ozaki, Yusuke; Sasao, Eiji

no journal, , 

no abstracts in English

Oral presentation

Comparison of geometric and hydraulic characteristics of fractures obtained from surface-based investigation and underground tunnel excavating investigations

Ishibashi, Masayuki*; Miyoshi, Takako*; Onoe, Hironori*; Masumoto, Kazuhiko*; Sasao, Eiji; Takeuchi, Ryuji

no journal, , 

no abstracts in English

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