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Conference Paper: From orogenic collapse to rifting, structures of the South China Sea

TitleFrom orogenic collapse to rifting, structures of the South China Sea
Authors
Issue Date2009
PublisherCopernicus GmbH. The Journal's web site is located at http://www.geophysical-research-abstracts.net
Citation
The 6th General Assembly of the European Geosciences Union (EGU 2009), Vienna, Austria, 19-24 April 2009. In Geophysical Research Abstracts, 2009, v. 11, no. EGU2009-11687 How to Cite?
AbstractThe opening of the South China Sea has been a matter of debate for many years because of its internal structure, the differences between the conjugate margins and the variations of rifting and spreading directions. Although it is considered as being a back-arc basin, it is not sitting directly above a subduction zone, and the rifting process lasted for an unusually long duration. Among the specific characteristics is the early phase of rifting which took place early in place of the former Yanshanian andean-type mountain range. This stage is marked by narrow basins filled with deformed conglomerate, and initiated around 70My ago within a framework where the oblique subduction …
Persistent Identifierhttp://hdl.handle.net/10722/64148
ISSN

 

DC FieldValueLanguage
dc.contributor.authorPubellier, Men_HK
dc.contributor.authorChan, LSen_HK
dc.contributor.authorChamot Rooke, Nen_HK
dc.contributor.authorShen, Wen_HK
dc.contributor.authorRingenbach, JCen_HK
dc.date.accessioned2010-07-13T04:41:28Z-
dc.date.available2010-07-13T04:41:28Z-
dc.date.issued2009en_HK
dc.identifier.citationThe 6th General Assembly of the European Geosciences Union (EGU 2009), Vienna, Austria, 19-24 April 2009. In Geophysical Research Abstracts, 2009, v. 11, no. EGU2009-11687-
dc.identifier.issn1607-7962-
dc.identifier.urihttp://hdl.handle.net/10722/64148-
dc.description.abstractThe opening of the South China Sea has been a matter of debate for many years because of its internal structure, the differences between the conjugate margins and the variations of rifting and spreading directions. Although it is considered as being a back-arc basin, it is not sitting directly above a subduction zone, and the rifting process lasted for an unusually long duration. Among the specific characteristics is the early phase of rifting which took place early in place of the former Yanshanian andean-type mountain range. This stage is marked by narrow basins filled with deformed conglomerate, and initiated around 70My ago within a framework where the oblique subduction …-
dc.languageengen_HK
dc.publisherCopernicus GmbH. The Journal's web site is located at http://www.geophysical-research-abstracts.net-
dc.relation.ispartofGeophysical Research Abstracts-
dc.rightsCreative Commons: Attribution 3.0 Hong Kong License-
dc.titleFrom orogenic collapse to rifting, structures of the South China Seaen_HK
dc.typeConference_Paperen_HK
dc.identifier.emailChan, LS: chanls@hku.hken_HK
dc.identifier.authorityChan, LS=rp00665en_HK
dc.description.naturepublished_or_final_version-
dc.identifier.hkuros166783en_HK
dc.identifier.volume11-
dc.publisher.placeGermany-

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