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Conference Paper: On Nature of Earthquakes with Cause of Compressed Methane Gas Expansion and Migration in Crustal Rocks

TitleOn Nature of Earthquakes with Cause of Compressed Methane Gas Expansion and Migration in Crustal Rocks
Authors
Issue Date2013
PublisherAmerican Society of Civil Engineers
Citation
5th Biot Conference on Poromechanics, Vienna, Austria, 10-12 July 2013. In Hellmich, C ... (et al) (Eds.), Poromechanics V: proceedings of the fifth Biot Conference on Poromechanics, July 10-12, 2013, Vienna, Austria, p. 507-516. Reston, Va.: American Society of Civil Engineers, 2013 How to Cite?
AbstractThis paper presents a hypothesis of compressed methane gas expansion and migration in crustal rocks and faults for the cause of earthquakes. An earth quaking is an adiabatic process of kinetic interaction between rapid upward expansion and migration of compressed natural gas and its surrounding crustal rocks and ground soils. The natural gas is produced in core and/or mantle. It is escaped from its traps in deep fault zones of the lower crustal rocks. The interaction is instantaneous and flashing. It can be complete within few to tens and to hundreds seconds. The gas expansion and migration are confined and constrained by the inward gravity, the tectonic stresses, and the rigidness and strengths of the crustal rocks. The kinetic energy of earth quaking is mainly the physical expansion energy of the highly compressed methane gas. The gas expansion work causing the 2008 Wenchuan Earthquake and the 2011 Off the Pacific Coast of Tohoku Earthquake are estimated.
Persistent Identifierhttp://hdl.handle.net/10722/190814
ISBN

 

DC FieldValueLanguage
dc.contributor.authorYue, QZQen_US
dc.date.accessioned2013-09-17T15:46:53Z-
dc.date.available2013-09-17T15:46:53Z-
dc.date.issued2013en_US
dc.identifier.citation5th Biot Conference on Poromechanics, Vienna, Austria, 10-12 July 2013. In Hellmich, C ... (et al) (Eds.), Poromechanics V: proceedings of the fifth Biot Conference on Poromechanics, July 10-12, 2013, Vienna, Austria, p. 507-516. Reston, Va.: American Society of Civil Engineers, 2013en_US
dc.identifier.isbn9780784412992en_US
dc.identifier.urihttp://hdl.handle.net/10722/190814-
dc.description.abstractThis paper presents a hypothesis of compressed methane gas expansion and migration in crustal rocks and faults for the cause of earthquakes. An earth quaking is an adiabatic process of kinetic interaction between rapid upward expansion and migration of compressed natural gas and its surrounding crustal rocks and ground soils. The natural gas is produced in core and/or mantle. It is escaped from its traps in deep fault zones of the lower crustal rocks. The interaction is instantaneous and flashing. It can be complete within few to tens and to hundreds seconds. The gas expansion and migration are confined and constrained by the inward gravity, the tectonic stresses, and the rigidness and strengths of the crustal rocks. The kinetic energy of earth quaking is mainly the physical expansion energy of the highly compressed methane gas. The gas expansion work causing the 2008 Wenchuan Earthquake and the 2011 Off the Pacific Coast of Tohoku Earthquake are estimated.-
dc.languageengen_US
dc.publisherAmerican Society of Civil Engineersen_US
dc.relation.ispartofPoromechanics V: proceedings of the fifth Biot Conference on Poromechanics, July 10-12, 2013, Vienna, Austriaen_US
dc.titleOn Nature of Earthquakes with Cause of Compressed Methane Gas Expansion and Migration in Crustal Rocksen_US
dc.typeConference_Paperen_US
dc.identifier.emailYue, QZQ: yueqzq@hku.hken_US
dc.identifier.authorityYue, QZQ=rp00209en_US
dc.identifier.doi10.1061/9780784412992.060-
dc.identifier.scopuseid_2-s2.0-84887386415-
dc.identifier.hkuros224817en_US
dc.identifier.spage507en_US
dc.identifier.epage516en_US
dc.publisher.placeReston, Va.-
dc.description.other5th Biot Conference on Poromechanics, Vienna, Austria, 10-12 July 2013. In Hellmich, C ... (et al) (Eds.), Poromechanics V: proceedings of the fifth Biot Conference on Poromechanics, July 10-12, 2013, Vienna, Austria, p. 507-516. Reston, Va.: American Society of Civil Engineers, 2013-

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