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Article: Palaeoproterozoic assembly of the North China Craton

TitlePalaeoproterozoic assembly of the North China Craton
Authors
Zhao, G
KeywordsEarth sciences
Geology
Issue Date2001
PublisherCambridge University Press. The Journal's web site is located at http://journals.cambridge.org/action/displayJournal?jid=GEO
Citation
Geological Magazine, 2001, v. 138 n. 1, p. 87-91 How to Cite?
DOI: http://dx.doi.org/10.1017/S0016756801005040
AbstractThe basement of the North China Craton consists of the Eastern and Western blocks, separated by the Central Zone. Both the Eastern and Western blocks are dominated by late Archaean tonalitic-trondhjemitic-granodioritic gneiss complexes interdigitated with minor supracrustal rocks metamorphosed at 2̃.5 Ga, with anticlockwise P-T paths. The Central Zone is composed of reworked late Archaean components and Palaeoproterozoic juvenile crustal materials that underwent regional metamorphism at 1̃.85 Ga, with clockwise P-T paths involving isothermal decompression as a result of collision between the Eastern and Western blocks, which resulted in the final assembly of the North China Craton.
Persistent Identifierhttp://hdl.handle.net/10722/42377
ISSN
0016-7568
2023 Impact Factor: 2.0
2023 SCImago Journal Rankings: 0.851
ISI Accession Number ID
WOS:000167421700007
References
References in Scopus

 

DC FieldValueLanguage
dc.contributor.authorZhao, Gen_HK
dc.date.accessioned2007-01-29T08:48:17Z-
dc.date.available2007-01-29T08:48:17Z-
dc.date.issued2001en_HK
dc.identifier.citationGeological Magazine, 2001, v. 138 n. 1, p. 87-91en_HK
dc.identifier.issn0016-7568en_HK
dc.identifier.urihttp://hdl.handle.net/10722/42377-
dc.description.abstractThe basement of the North China Craton consists of the Eastern and Western blocks, separated by the Central Zone. Both the Eastern and Western blocks are dominated by late Archaean tonalitic-trondhjemitic-granodioritic gneiss complexes interdigitated with minor supracrustal rocks metamorphosed at 2̃.5 Ga, with anticlockwise P-T paths. The Central Zone is composed of reworked late Archaean components and Palaeoproterozoic juvenile crustal materials that underwent regional metamorphism at 1̃.85 Ga, with clockwise P-T paths involving isothermal decompression as a result of collision between the Eastern and Western blocks, which resulted in the final assembly of the North China Craton.en_HK
dc.format.extent217162 bytes-
dc.format.extent25088 bytes-
dc.format.mimetypeapplication/pdf-
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dc.languageengen_HK
dc.publisherCambridge University Press. The Journal's web site is located at http://journals.cambridge.org/action/displayJournal?jid=GEOen_HK
dc.relation.ispartofGeological Magazineen_HK
dc.rightsGeological Magazine. Copyright © Cambridge University Press.en_HK
dc.subjectEarth sciencesen_HK
dc.subjectGeologyen_HK
dc.titlePalaeoproterozoic assembly of the North China Cratonen_HK
dc.typeArticleen_HK
dc.identifier.openurlhttp://library.hku.hk:4550/resserv?sid=HKU:IR&issn=0016-7568&volume=138&issue=1&spage=87&epage=91&date=2001&atitle=Palaeoproterozoic+assembly+of+the+North+China+Cratonen_HK
dc.identifier.emailZhao, G:gzhao@hkucc.hku.hken_HK
dc.identifier.authorityZhao, G=rp00842en_HK
dc.description.naturepublished_or_final_versionen_HK
dc.identifier.doi10.1017/S0016756801005040en_HK
dc.identifier.scopuseid_2-s2.0-0035052305en_HK
dc.identifier.hkuros57268-
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-0035052305&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume138en_HK
dc.identifier.issue1en_HK
dc.identifier.spage87en_HK
dc.identifier.epage91en_HK
dc.identifier.isiWOS:000167421700007-
dc.publisher.placeUnited Kingdomen_HK
dc.identifier.scopusauthoridZhao, G=7403296321en_HK
dc.identifier.issnl0016-7568-

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