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Article: Deformation history of the Hengshan Complex: Implications for the tectonic evolution of the Trans-North China Orogen

TitleDeformation history of the Hengshan Complex: Implications for the tectonic evolution of the Trans-North China Orogen
Authors
KeywordsArchaean
Deformation
Hengshan Complex
North China Craton
Palaeoproterozoic
Trans-North China Orogen
Issue Date2007
PublisherPergamon. The Journal's web site is located at http://www.elsevier.com/locate/jsg
Citation
Journal Of Structural Geology, 2007, v. 29 n. 6, p. 933-949 How to Cite?
AbstractStructural analysis indicates that the Hengshan Complex underwent five distinct episodes of deformation (D 1-D 5). The D 1 episode formed small isoclinal folds (F 1), penetrative axial planar foliations (S 1) and mineral stretching lineations (L 1). D 1 fabrics were reworked by following D 2 deformation. Associated with D 2 was the development of NW-verging asymmetric folds and accompanying thrust faults. Both D 1 and D 2 resulted from crustal thickening and coherent with prograde and peak metamorphism. D 2 deformation was followed by transpressional dextral shearing (D 3), including top-to-NW oblique-slip shearing and NNE-SSW dextral strike-slip shearing. Ongoing collision led to development of the Zhujiafang ductile shear zone (D 4), a near E-W trending high strain belt across the Hengshan Complex. D 5 deformation is characterized by F 5 open folds and associated normal faults, probably related to exhumation of the complex. Structural patterns of the Hengshan Complex can place important insights into a recently proposed tectonic model suggesting that an ocean between the Eastern and Western Blocks underwent eastward-directed subduction beneath the western margin of the Eastern Block, and closure of this ocean finally led to collision between the two blocks to form the coherent North China Craton. © 2007 Elsevier Ltd. All rights reserved.
Persistent Identifierhttp://hdl.handle.net/10722/73096
ISSN
2015 Impact Factor: 2.084
2015 SCImago Journal Rankings: 1.648
ISI Accession Number ID
References

 

DC FieldValueLanguage
dc.contributor.authorZhang, Jen_HK
dc.contributor.authorZhao, Gen_HK
dc.contributor.authorLi, Sen_HK
dc.contributor.authorSun, Men_HK
dc.contributor.authorLiu, Sen_HK
dc.contributor.authorWilde, SAen_HK
dc.contributor.authorKröner, Aen_HK
dc.contributor.authorYin, Cen_HK
dc.date.accessioned2010-09-06T06:48:00Z-
dc.date.available2010-09-06T06:48:00Z-
dc.date.issued2007en_HK
dc.identifier.citationJournal Of Structural Geology, 2007, v. 29 n. 6, p. 933-949en_HK
dc.identifier.issn0191-8141en_HK
dc.identifier.urihttp://hdl.handle.net/10722/73096-
dc.description.abstractStructural analysis indicates that the Hengshan Complex underwent five distinct episodes of deformation (D 1-D 5). The D 1 episode formed small isoclinal folds (F 1), penetrative axial planar foliations (S 1) and mineral stretching lineations (L 1). D 1 fabrics were reworked by following D 2 deformation. Associated with D 2 was the development of NW-verging asymmetric folds and accompanying thrust faults. Both D 1 and D 2 resulted from crustal thickening and coherent with prograde and peak metamorphism. D 2 deformation was followed by transpressional dextral shearing (D 3), including top-to-NW oblique-slip shearing and NNE-SSW dextral strike-slip shearing. Ongoing collision led to development of the Zhujiafang ductile shear zone (D 4), a near E-W trending high strain belt across the Hengshan Complex. D 5 deformation is characterized by F 5 open folds and associated normal faults, probably related to exhumation of the complex. Structural patterns of the Hengshan Complex can place important insights into a recently proposed tectonic model suggesting that an ocean between the Eastern and Western Blocks underwent eastward-directed subduction beneath the western margin of the Eastern Block, and closure of this ocean finally led to collision between the two blocks to form the coherent North China Craton. © 2007 Elsevier Ltd. All rights reserved.en_HK
dc.languageengen_HK
dc.publisherPergamon. The Journal's web site is located at http://www.elsevier.com/locate/jsgen_HK
dc.relation.ispartofJournal of Structural Geologyen_HK
dc.subjectArchaeanen_HK
dc.subjectDeformationen_HK
dc.subjectHengshan Complexen_HK
dc.subjectNorth China Cratonen_HK
dc.subjectPalaeoproterozoicen_HK
dc.subjectTrans-North China Orogenen_HK
dc.titleDeformation history of the Hengshan Complex: Implications for the tectonic evolution of the Trans-North China Orogenen_HK
dc.typeArticleen_HK
dc.identifier.openurlhttp://library.hku.hk:4550/resserv?sid=HKU:IR&issn=0191-8141&volume=29&issue=6&spage=933&epage=949&date=2007&atitle=Deformation+history+of+the+Hengshan+Complex:+implications+for+the+tectonic+evolution+of+the+Trans-North+China+Orogenen_HK
dc.identifier.emailZhao, G:gzhao@hkucc.hku.hken_HK
dc.identifier.emailSun, M:minsun@hku.hken_HK
dc.identifier.authorityZhao, G=rp00842en_HK
dc.identifier.authoritySun, M=rp00780en_HK
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1016/j.jsg.2007.02.013en_HK
dc.identifier.scopuseid_2-s2.0-34248682965en_HK
dc.identifier.hkuros127569en_HK
dc.identifier.hkuros194902-
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-34248682965&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume29en_HK
dc.identifier.issue6en_HK
dc.identifier.spage933en_HK
dc.identifier.epage949en_HK
dc.identifier.isiWOS:000247357300003-
dc.publisher.placeUnited Kingdomen_HK
dc.identifier.scopusauthoridZhang, J=49061670600en_HK
dc.identifier.scopusauthoridZhao, G=7403296321en_HK
dc.identifier.scopusauthoridLi, S=8784176300en_HK
dc.identifier.scopusauthoridSun, M=25932315800en_HK
dc.identifier.scopusauthoridLiu, S=35253878000en_HK
dc.identifier.scopusauthoridWilde, SA=35254758600en_HK
dc.identifier.scopusauthoridKröner, A=7006453132en_HK
dc.identifier.scopusauthoridYin, C=16053843700en_HK

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