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Article: Origin and geological significance of Paleoproterozoic granites in the northeastern Cathaysia Block, South China

TitleOrigin and geological significance of Paleoproterozoic granites in the northeastern Cathaysia Block, South China
Authors
KeywordsArchean basement
Geochemistry of granites
Northeastern cathaysia block
Paleoproterozoic orogeny
Zircon U-Pb-Hf isotopes
Issue Date2014
PublisherElsevier BV. The Journal's web site is located at http://www.elsevier.com/locate/precamres
Citation
Precambrian Research, 2014, v. 248, p. 72-95 How to Cite?
Persistent Identifierhttp://hdl.handle.net/10722/216912
ISSN
2020 Impact Factor: 4.725
2015 SCImago Journal Rankings: 3.214
ISI Accession Number ID

 

DC FieldValueLanguage
dc.contributor.authorLiu, Q-
dc.contributor.authorYu, JH-
dc.contributor.authorO’Reilly, SY-
dc.contributor.authorZhou, MF-
dc.contributor.authorGriffin, WL-
dc.contributor.authorWang, L-
dc.contributor.authorCui, X-
dc.date.accessioned2015-09-18T05:42:49Z-
dc.date.available2015-09-18T05:42:49Z-
dc.date.issued2014-
dc.identifier.citationPrecambrian Research, 2014, v. 248, p. 72-95-
dc.identifier.issn0301-9268-
dc.identifier.urihttp://hdl.handle.net/10722/216912-
dc.languageeng-
dc.publisherElsevier BV. The Journal's web site is located at http://www.elsevier.com/locate/precamres-
dc.relation.ispartofPrecambrian Research-
dc.subjectArchean basement-
dc.subjectGeochemistry of granites-
dc.subjectNortheastern cathaysia block-
dc.subjectPaleoproterozoic orogeny-
dc.subjectZircon U-Pb-Hf isotopes-
dc.titleOrigin and geological significance of Paleoproterozoic granites in the northeastern Cathaysia Block, South China-
dc.typeArticle-
dc.identifier.emailZhou, MF: mfzhou@hku.hk-
dc.identifier.authorityZhou, MF=rp00844-
dc.identifier.doi10.1016/j.precamres.2014.04.001-
dc.identifier.scopuseid_2-s2.0-84900514202-
dc.identifier.hkuros255070-
dc.identifier.volume248-
dc.identifier.spage72-
dc.identifier.epage95-
dc.identifier.isiWOS:000338620000005-
dc.publisher.placeNetherlands-
dc.identifier.issnl0301-9268-

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