Non-tectonic faults due to landslide movement and their mechanism
نویسندگان
چکیده
منابع مشابه
Fabric induced weakness of tectonic faults
[1] Mature fault zones appear to be weaker than predicted by both theory and experiment. One explanation involves the presence of weak minerals, such as talc. However, talc is only a minor constituent of most fault zones and thus the question arises: what proportion of a weak mineral is needed to satisfy weak fault models? Existing studies of fault gouges indicate that >30% of the weak phase is...
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15 صفحه اولUncertainty due to DEM error in landslide susceptibility mapping
A-Xing ZHU * 21 State Key Laboratory of Resources and Environmental Information System, Institute 22 of Geographical Sciences and Natural Resources Research, CAS, Beijing 100101, 23 China 24 and 25 Department of geography, University of Wisconsin Madison, 550N, Park Street, 26 Madison, WI 53706-1491, USA 27 * Corresponding author. Phone: 86-10-64888961. Fax: 86-10-64889630. Email: 28 axing@lrei...
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ژورنال
عنوان ژورنال: Journal of the Japan Landslide Society
سال: 2007
ISSN: 1882-0034,1348-3986
DOI: 10.3313/jls.44.205