File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

Article: Cause and mechanism of highly compressed and dense methane gas mass for Wenchuan Earthquake and associated rock-avalanches and surface co-seismic ruptures

TitleCause and mechanism of highly compressed and dense methane gas mass for Wenchuan Earthquake and associated rock-avalanches and surface co-seismic ruptures
汶川地震与山崩地裂的极高压甲烷天然气成因和机理
Authors
KeywordsCause and mechanism
Dense methane gas
Rock avalanches
Wenchuan earthquake
Issue Date2013
PublisherChina University of Geosciences and Peking University. The Journal's web site is located at http://dxqy.chinajournal.net.cn/
Citation
Earth Science Frontiers, 2013, v. 20 n. 6, p. 15-20 How to Cite?
地學前縁, 2013, v. 20 n. 6, p. 15-20 How to Cite?
AbstractThis paper presents and shows that Wenchuan Earthquake of May 12, 2008 was caused by the rapid migration and expansion of a large amount of highly pressurized and dense methane gas mass in crustal rock masses. The dense gas mass was trapped in deep crustal rock masses. Because of increase in its pressure and mass, the dense gas mass suddenly ruptured the crustal rocks at deep Longmenshan faults with high compressions. A part of the dense gas mass escaped the trap and rapidly migrated from deep crustal rock to shallow crustal rocks along the faults, contacts and beddings and expanded the crustal rock masses. The expanding power of the dense gas that migrated into some isolated hard rock slopes caused the rock avalanche-rock debris flows at mountains. The expanding power of the dense gas that migrated into some isolated soil river beds and slopes caused the co-seismic ruptures at ground surfaces.
Persistent Identifierhttp://hdl.handle.net/10722/202626
ISSN
2023 SCImago Journal Rankings: 0.413

 

DC FieldValueLanguage
dc.contributor.authorYue, QZQen_US
dc.date.accessioned2014-09-19T09:14:07Z-
dc.date.available2014-09-19T09:14:07Z-
dc.date.issued2013en_US
dc.identifier.citationEarth Science Frontiers, 2013, v. 20 n. 6, p. 15-20en_US
dc.identifier.citation地學前縁, 2013, v. 20 n. 6, p. 15-20en_US
dc.identifier.issn1005-2321-
dc.identifier.urihttp://hdl.handle.net/10722/202626-
dc.description.abstractThis paper presents and shows that Wenchuan Earthquake of May 12, 2008 was caused by the rapid migration and expansion of a large amount of highly pressurized and dense methane gas mass in crustal rock masses. The dense gas mass was trapped in deep crustal rock masses. Because of increase in its pressure and mass, the dense gas mass suddenly ruptured the crustal rocks at deep Longmenshan faults with high compressions. A part of the dense gas mass escaped the trap and rapidly migrated from deep crustal rock to shallow crustal rocks along the faults, contacts and beddings and expanded the crustal rock masses. The expanding power of the dense gas that migrated into some isolated hard rock slopes caused the rock avalanche-rock debris flows at mountains. The expanding power of the dense gas that migrated into some isolated soil river beds and slopes caused the co-seismic ruptures at ground surfaces.en_US
dc.languagechien_US
dc.publisherChina University of Geosciences and Peking University. The Journal's web site is located at http://dxqy.chinajournal.net.cn/en_US
dc.relation.ispartofEarth Science Frontiersen_US
dc.relation.ispartof地學前縁en_US
dc.subjectCause and mechanism-
dc.subjectDense methane gas-
dc.subjectRock avalanches-
dc.subjectWenchuan earthquake-
dc.titleCause and mechanism of highly compressed and dense methane gas mass for Wenchuan Earthquake and associated rock-avalanches and surface co-seismic rupturesen_US
dc.title汶川地震与山崩地裂的极高压甲烷天然气成因和机理en_US
dc.typeArticleen_US
dc.identifier.emailYue, QZQ: yueqzq@hku.hken_US
dc.identifier.authorityYue, QZQ=rp00209en_US
dc.identifier.scopuseid_2-s2.0-84890839548-
dc.identifier.hkuros235660en_US
dc.identifier.volume20en_US
dc.identifier.issue6en_US
dc.identifier.spage15en_US
dc.identifier.epage20en_US
dc.publisher.placeBeijing, Chinaen_US
dc.identifier.issnl1005-2321-

Export via OAI-PMH Interface in XML Formats


OR


Export to Other Non-XML Formats