File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

Article: Mesozoic basins in eastern China and their bearing on the deconstruction of the North China Craton

TitleMesozoic basins in eastern China and their bearing on the deconstruction of the North China Craton
Authors
Issue Date2012
PublisherPergamon. The Journal's web site is located at http://www.elsevier.com/locate/jseaes
Citation
Journal of Asian Earth Sciences, 2012, v. 47, p. 64-79 How to Cite?
AbstractMesozoic basins occur widely in the Eastern Block and the neighboring area of the North China Craton, including the Bohai Bay, the Jiaolai, the Hefei and the North Yellow Sea in the north, and the Jianghan and the Subei-South Yellow Sea basins to the south. Their spatial-temporal framework is the consequence of the Indosinian and Yanshanian tectonic regimes in eastern China and record the events related to Mesozoic deconstruction of the North China Craton. Our results demonstrate that the Mesozoic tectonic evolution of the eastern North China Craton was related to both sub-crustal delamination and intra-crustal extrusion or escape tectonics. Thus, we propose that the mechanism of uplift of the Yanshanian North China Plateau and related lithosphere thinning in the eastern North China Craton were related to sub-crustal delamination at depth. However, the different distribution patterns of the basins on both sides of the Tan-Lu Fault System as well as the co-existence of both compressional and extensional basins in the Mesozoic indicate that these were controlled by escape tectonics in different tectonic parts of the crust. © 2011 Elsevier Ltd.
Persistent Identifierhttp://hdl.handle.net/10722/151360
ISSN
2015 Impact Factor: 2.647
2015 SCImago Journal Rankings: 1.393
ISI Accession Number ID
Funding AgencyGrant Number
China Geological Survey Bureau1212011120103
NSFC41072152
90814011
S8632009AA093401
Funding Information:

The reviews of JAES referees, Profs. Yongjiang Liu and Yunpeng Dong were very helpful in improving and earlier version of this manuscript. This research was financially supported by Project (1212011120103) of China Geological Survey Bureau, S863 (2009AA093401), the NSFC (Grants 41072152, 90814011). Writing of this manuscript was done when Sanzhong Li was a Guest Investigator at the Woods Hole Oceanographic Institution (WHOI). We thank Prof. Lin Jian help us improve our initial manuscript.

References

 

DC FieldValueLanguage
dc.contributor.authorLi, Sen_US
dc.contributor.authorZhao, Gen_US
dc.contributor.authorDai, Len_US
dc.contributor.authorLiu, Xen_US
dc.contributor.authorZhou, Len_US
dc.contributor.authorSantosh, Men_US
dc.contributor.authorSuo, Yen_US
dc.date.accessioned2012-06-26T06:21:07Z-
dc.date.available2012-06-26T06:21:07Z-
dc.date.issued2012en_US
dc.identifier.citationJournal of Asian Earth Sciences, 2012, v. 47, p. 64-79en_US
dc.identifier.issn1367-9120en_US
dc.identifier.urihttp://hdl.handle.net/10722/151360-
dc.description.abstractMesozoic basins occur widely in the Eastern Block and the neighboring area of the North China Craton, including the Bohai Bay, the Jiaolai, the Hefei and the North Yellow Sea in the north, and the Jianghan and the Subei-South Yellow Sea basins to the south. Their spatial-temporal framework is the consequence of the Indosinian and Yanshanian tectonic regimes in eastern China and record the events related to Mesozoic deconstruction of the North China Craton. Our results demonstrate that the Mesozoic tectonic evolution of the eastern North China Craton was related to both sub-crustal delamination and intra-crustal extrusion or escape tectonics. Thus, we propose that the mechanism of uplift of the Yanshanian North China Plateau and related lithosphere thinning in the eastern North China Craton were related to sub-crustal delamination at depth. However, the different distribution patterns of the basins on both sides of the Tan-Lu Fault System as well as the co-existence of both compressional and extensional basins in the Mesozoic indicate that these were controlled by escape tectonics in different tectonic parts of the crust. © 2011 Elsevier Ltd.en_US
dc.languageengen_US
dc.publisherPergamon. The Journal's web site is located at http://www.elsevier.com/locate/jseaesen_US
dc.relation.ispartofJournal of Asian Earth Sciencesen_US
dc.subject.meshDelamination-
dc.subject.meshExtrusion-
dc.subject.meshMesozoic-
dc.subject.meshSpatiotemporal analysis-
dc.subject.meshTectonic evolution-
dc.titleMesozoic basins in eastern China and their bearing on the deconstruction of the North China Cratonen_US
dc.typeArticleen_US
dc.identifier.emailLi, S: Sanzhong@ouc.edu.cnen_US
dc.identifier.emailZhao, G: gzhao@hkucc.hku.hk-
dc.identifier.authorityZhao, G=rp00842en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.doi10.1016/j.jseaes.2011.06.008en_US
dc.identifier.scopuseid_2-s2.0-84857532515en_US
dc.identifier.hkuros204273-
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-84857532515&selection=ref&src=s&origin=recordpageen_US
dc.identifier.volume47en_US
dc.identifier.spage64en_US
dc.identifier.epage79en_US
dc.identifier.isiWOS:000302756200006-
dc.publisher.placeUnited Kingdomen_US
dc.identifier.scopusauthoridSuo, Y=36543084000en_US
dc.identifier.scopusauthoridSantosh, M=7005398812en_US
dc.identifier.scopusauthoridZhou, L=25930169500en_US
dc.identifier.scopusauthoridLiu, X=36675133800en_US
dc.identifier.scopusauthoridDai, L=36174941600en_US
dc.identifier.scopusauthoridZhao, G=7403296321en_US
dc.identifier.scopusauthoridLi, S=35248444400en_US
dc.identifier.citeulike9534757-

Export via OAI-PMH Interface in XML Formats


OR


Export to Other Non-XML Formats