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Article: Mesozoic extensional structures of the Fangshan tectonic dome and their subsequent reworking during collisional accretion of the North China Block

TitleMesozoic extensional structures of the Fangshan tectonic dome and their subsequent reworking during collisional accretion of the North China Block
Authors
Issue Date2006
PublisherGeological Society Publishing House. The Journal's web site is located at http://www.geolsoc.org.uk/gsl/publications/journals/jgs
Citation
Journal Of The Geological Society, 2006, v. 163 n. 1, p. 127-142 How to Cite?
AbstractThe Fangshan area, SW of Beijing, lies at the junction of the NNE-trending Taihang mountain range and the southeastern portion of the Yanshan intraplate orogenic belt and has undergone at least five stages of deformation. Mid- to late Triassic extensional deformation (D1) is represented by the formation of the Fangshan tectonic dome during SE-directed extensional tectonics. This deformation was later modified by NNW-directed thrusting in the late Triassic (D2) and WNW-directed thrusting in the late Jurassic (D3). These D1-D3 structures were deformed by the arcuate Beiling syncline (D4), which formed during the intrusion of the 133-128 Ma Fangshan pluton. D5 deformation is represented by Cretaceous to Quaternary NNE-striking high-angle normal faults. The ages of these events demonstrate that the principal ENE-trending tectonic framework of the Yanshan intraplate orogenic belt was established mainly in the mid- to late Triassic (the Indosinian event). The Jurassic to Cretaceous Yanshanian deformation with thick-skinned thrusting was associated with intrusion of numerous plutons, and strongly modified the older structures. The tectonic evolution of the Fangshan tectonic dome was linked genetically with the collision of the North China Block and the Siberian Craton, and the later collision of the North and South China blocks.
Persistent Identifierhttp://hdl.handle.net/10722/72636
ISSN
2015 Impact Factor: 2.473
2015 SCImago Journal Rankings: 1.449
ISI Accession Number ID
References

 

DC FieldValueLanguage
dc.contributor.authorYan, DPen_HK
dc.contributor.authorZhou, MFen_HK
dc.contributor.authorSong, HLen_HK
dc.contributor.authorWang, GHen_HK
dc.contributor.authorSun, Men_HK
dc.date.accessioned2010-09-06T06:43:41Z-
dc.date.available2010-09-06T06:43:41Z-
dc.date.issued2006en_HK
dc.identifier.citationJournal Of The Geological Society, 2006, v. 163 n. 1, p. 127-142en_HK
dc.identifier.issn0016-7649en_HK
dc.identifier.urihttp://hdl.handle.net/10722/72636-
dc.description.abstractThe Fangshan area, SW of Beijing, lies at the junction of the NNE-trending Taihang mountain range and the southeastern portion of the Yanshan intraplate orogenic belt and has undergone at least five stages of deformation. Mid- to late Triassic extensional deformation (D1) is represented by the formation of the Fangshan tectonic dome during SE-directed extensional tectonics. This deformation was later modified by NNW-directed thrusting in the late Triassic (D2) and WNW-directed thrusting in the late Jurassic (D3). These D1-D3 structures were deformed by the arcuate Beiling syncline (D4), which formed during the intrusion of the 133-128 Ma Fangshan pluton. D5 deformation is represented by Cretaceous to Quaternary NNE-striking high-angle normal faults. The ages of these events demonstrate that the principal ENE-trending tectonic framework of the Yanshan intraplate orogenic belt was established mainly in the mid- to late Triassic (the Indosinian event). The Jurassic to Cretaceous Yanshanian deformation with thick-skinned thrusting was associated with intrusion of numerous plutons, and strongly modified the older structures. The tectonic evolution of the Fangshan tectonic dome was linked genetically with the collision of the North China Block and the Siberian Craton, and the later collision of the North and South China blocks.en_HK
dc.languageengen_HK
dc.publisherGeological Society Publishing House. The Journal's web site is located at http://www.geolsoc.org.uk/gsl/publications/journals/jgsen_HK
dc.relation.ispartofJournal of the Geological Societyen_HK
dc.titleMesozoic extensional structures of the Fangshan tectonic dome and their subsequent reworking during collisional accretion of the North China Blocken_HK
dc.typeArticleen_HK
dc.identifier.openurlhttp://library.hku.hk:4550/resserv?sid=HKU:IR&issn=0016-7649&volume=163&spage=127&epage=142&date=2006&atitle=Mesozoic+extensional+structures+of+the+Fangshan+tectonic+dome+and+their+subsequent+reworking+during+collisional+accretion+of+the+North+China+Block-
dc.identifier.emailZhou, MF:mfzhou@hkucc.hku.hken_HK
dc.identifier.emailSun, M:minsun@hku.hken_HK
dc.identifier.authorityZhou, MF=rp00844en_HK
dc.identifier.authoritySun, M=rp00780en_HK
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1144/0016-764904-154en_HK
dc.identifier.scopuseid_2-s2.0-29244480299en_HK
dc.identifier.hkuros120039en_HK
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-29244480299&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume163en_HK
dc.identifier.issue1en_HK
dc.identifier.spage127en_HK
dc.identifier.epage142en_HK
dc.identifier.isiWOS:000234308300012-
dc.publisher.placeUnited Kingdomen_HK
dc.identifier.scopusauthoridYan, DP=36683417500en_HK
dc.identifier.scopusauthoridZhou, MF=7403506005en_HK
dc.identifier.scopusauthoridSong, HL=47261333700en_HK
dc.identifier.scopusauthoridWang, GH=14122606700en_HK
dc.identifier.scopusauthoridSun, M=25932315800en_HK
dc.identifier.citeulike421090-

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