In‐situ stress at a site close proximity to the Gofukuji Fault, central Japan, measured using drilling cores-Reference-Cited by-同舟云学术

In‐situ stress at a site close proximity to the Gofukuji Fault, central Japan, measured using drilling cores

Published:2011-02-15 Issue:2 Volume:20 Page:160-173
ISSN:1038-4871
Container-title:Island Arc
language:en
Short-container-title:Island Arc

Author:

YABE YASUO¹,OMURA KENTARO²

Affiliation:

1. Research Center for Prediction of Earthquakes and Volcanic Eruptions, Graduate School of Science, Tohoku University, Sendai, Miyagi 980‐8578, Japan (email: )

2. National Research Institute for Earth Science and Disaster Prevention, Tsukuba, Ibaraki 305‐0006, Japan

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1440-1738.2010.00756.x

Reference28 articles.

1. Drilling-induced tensile wall-fractures: implications for determination of in-situ stress orientation and magnitude

2. Friction of rocks

3. Time-dependent friction in rocks

4. GeologicalSurvey ofJapan AIST.2010.Seamless digital geological map of Japan 1:200 000. Feb 1 2010 version. Research Information Database DB084 Geological Survey of Japan National Institute of Advanced Industrial Science and Technology [online]. [Cited 15 Jun 2010.] Available from:http://riodb02.ibase.aist.go.jp/db084/

5. Headquarters forEarthquakeResearchPromotion1996.On research and evaluation of the Itoigawa‐Shizuoka Tectonic Line fault system [online]. [Cited 25 May 2010.] Available from:http://www.jishin.go.jp/main/chousa/katsudansou_pdf/41_42_44_itoigawa‐shizuoka.pdf(in Japanese).

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