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Keywords: rupture
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Proceedings Papers
Paper presented at the ISRM International Symposium on In-Situ Rock Stress, May 10–12, 2016
Paper Number: ISRM-ISRS-2016-009
... Abstract The Wenchuan Ms 8.0 earthquake occurred on the middle section of the Longmen-shan thrust belt, along the eastern border of the Tibetan Plateau. It ruptured simultaneously along two subparallel imbricated reverse faults, and they are Yingxiu-Baichuan fault and Guanxian-Jiangyou fault...
Proceedings Papers
Paper presented at the ISRM International Symposium on In-Situ Rock Stress, August 25–27, 2010
Paper Number: ISRM-ISRS-2010-080
... ABSTRACT: Non-mining rupture of coal mine shaft is a new kind of mine geological disaster. There are some standpoints on the reason of the shaft lining rupture, but a new option that the horizontal tectonic stresses lead to the rupture of the mine shaft is appeared after the shaft lining...
Proceedings Papers
Paper presented at the ISRM International Symposium on In-Situ Rock Stress, August 25–27, 2010
Paper Number: ISRM-ISRS-2010-124
... ABSTRACT: This paper summarizes the typical features and their regularities of the observed coseismic surface ruptures by Wenchuan Earthquake in terms of the three faults, ground locations, ground geomaterials, rupture geometries and rupture displacements. The paper then uses both...
Proceedings Papers
Paper presented at the ISRM International Symposium on In-Situ Rock Stress, August 25–27, 2010
Paper Number: ISRM-ISRS-2010-085
...°) reverse faults. The surface rupture is ∼240 km long with maximum vertical offset ∼9.0m and ∼4.9m right-slip. More than 80,000 people were killed, and over 370,000 people injured in the earthquake. It is the most disastrous event in China since the 1976 Tangshan earthquake, which killed more than 240,000...
Proceedings Papers
Paper presented at the ISRM International Symposium on In-Situ Rock Stress, August 25–27, 2010
Paper Number: ISRM-ISRS-2010-116
... ABSTRACT: The 2008 Wenchuan earthquake, Mw 7.9, ruptured the Longmenshan fault zone at the eastern margin of Tibetan Plateau and formed a 240-km-long surface rupture zone along the Yingxiu-Beichuan fault and an additional 70-km-long surface rupture zone along the Guanxian-Jiangyou fault. Some...