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Article: Isotopic chronology and geological events of Precambrian complex in Taihangshan region

TitleIsotopic chronology and geological events of Precambrian complex in Taihangshan region
Authors
KeywordsGeological Events
Isotopic Chronology
Precambrian Complex
Taihangshan Region
Issue Date2000
Publisher中國科學院. The Journal's web site is located at http://jdxg.chinajournal.net.cn/
Citation
Science In China, Series D: Earth Sciences, 2000, v. 43 n. 4, p. 386-393 How to Cite?
AbstractThere are five major geological events in Precambrian complex, Taihangshan region determined by researching into geology and isotopic chronology of the complex. Basaltic magma erupted and quartz-dioritic to tonalitic magma intruded in earlier neo-Archaean, which formed hornblende-plagiogneiss of Fuping gneiss complex and metamorphic mafic rock enclaves in TTG gneiss complex. Granulite facies metamorphism and emplacement of biotite-plagiogneiss occurred in late neo-Archaean. Extension and uplifting from the end of neo-Archaean to Paleoproterozoic era formed Chengnanzhuang large extensional deformation zones and metamorphic mafic veins emplaced into the deformation zones. Remobilization of Precambrian complex and tectonic uplifting in late Paleoproterozoic era formed Longquanguan ductile shear zone and emplacement of Nanying gneiss. Occurrence of regional granite pegmatite at the end of Paleoproterozoic era means the end of the Luliang movement.
Persistent Identifierhttp://hdl.handle.net/10722/151029
ISSN
2011 Impact Factor: 1.588
References

 

DC FieldValueLanguage
dc.contributor.authorLiu, Sen_US
dc.contributor.authorLiang, Hen_US
dc.contributor.authorZhao, Gen_US
dc.contributor.authorHua, Yen_US
dc.contributor.authorJian, Aen_US
dc.date.accessioned2012-06-26T06:16:10Z-
dc.date.available2012-06-26T06:16:10Z-
dc.date.issued2000en_US
dc.identifier.citationScience In China, Series D: Earth Sciences, 2000, v. 43 n. 4, p. 386-393en_US
dc.identifier.issn1006-9313en_US
dc.identifier.urihttp://hdl.handle.net/10722/151029-
dc.description.abstractThere are five major geological events in Precambrian complex, Taihangshan region determined by researching into geology and isotopic chronology of the complex. Basaltic magma erupted and quartz-dioritic to tonalitic magma intruded in earlier neo-Archaean, which formed hornblende-plagiogneiss of Fuping gneiss complex and metamorphic mafic rock enclaves in TTG gneiss complex. Granulite facies metamorphism and emplacement of biotite-plagiogneiss occurred in late neo-Archaean. Extension and uplifting from the end of neo-Archaean to Paleoproterozoic era formed Chengnanzhuang large extensional deformation zones and metamorphic mafic veins emplaced into the deformation zones. Remobilization of Precambrian complex and tectonic uplifting in late Paleoproterozoic era formed Longquanguan ductile shear zone and emplacement of Nanying gneiss. Occurrence of regional granite pegmatite at the end of Paleoproterozoic era means the end of the Luliang movement.en_US
dc.languageengen_US
dc.publisher中國科學院. The Journal's web site is located at http://jdxg.chinajournal.net.cn/zh_HK
dc.relation.ispartofScience in China, Series D: Earth Sciencesen_US
dc.subjectGeological Eventsen_US
dc.subjectIsotopic Chronologyen_US
dc.subjectPrecambrian Complexen_US
dc.subjectTaihangshan Regionen_US
dc.titleIsotopic chronology and geological events of Precambrian complex in Taihangshan regionen_US
dc.typeArticleen_US
dc.identifier.emailZhao, G:gzhao@hkucc.hku.hken_US
dc.identifier.authorityZhao, G=rp00842en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.scopuseid_2-s2.0-0033783719en_US
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-0033783719&selection=ref&src=s&origin=recordpageen_US
dc.identifier.volume43en_US
dc.identifier.issue4en_US
dc.identifier.spage386en_US
dc.identifier.epage393en_US
dc.publisher.placeChinaen_US
dc.identifier.scopusauthoridLiu, S=8287444600en_US
dc.identifier.scopusauthoridLiang, H=7402854175en_US
dc.identifier.scopusauthoridZhao, G=7403296321en_US
dc.identifier.scopusauthoridHua, Y=7203055092en_US
dc.identifier.scopusauthoridJian, A=36903530500en_US

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