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Article: Geochronology and geochemistry of meta-mafic dykes in the Quanji Massif, NW China: Paleoproterozoic evolution of the Tarim Craton and implications for the assembly of the Columbia supercontinent

TitleGeochronology and geochemistry of meta-mafic dykes in the Quanji Massif, NW China: Paleoproterozoic evolution of the Tarim Craton and implications for the assembly of the Columbia supercontinent
Authors
Liao, FZhang, LChen, NSun, MSantosh, MWang, QHMustafa, HA
KeywordsAmphibolites
Columbia supercontinent
Geochemistry
Mafic dyke
Tectonic evolution
Zircon U-Pb geochronology
Issue Date2014
Citation
Precambrian Research, 2014, v. 249, p. 33-56 How to Cite?
DOI: http://dx.doi.org/10.1016/j.precamres.2014.04.015
Persistent Identifierhttp://hdl.handle.net/10722/216877
ISI Accession Number ID
WOS:000339038100003

 

DC FieldValueLanguage
dc.contributor.authorLiao, F-
dc.contributor.authorZhang, L-
dc.contributor.authorChen, N-
dc.contributor.authorSun, M-
dc.contributor.authorSantosh, M-
dc.contributor.authorWang, QH-
dc.contributor.authorMustafa, HA-
dc.date.accessioned2015-09-18T05:41:53Z-
dc.date.available2015-09-18T05:41:53Z-
dc.date.issued2014-
dc.identifier.citationPrecambrian Research, 2014, v. 249, p. 33-56-
dc.identifier.urihttp://hdl.handle.net/10722/216877-
dc.languageeng-
dc.relation.ispartofPrecambrian Research-
dc.subjectAmphibolites-
dc.subjectColumbia supercontinent-
dc.subjectGeochemistry-
dc.subjectMafic dyke-
dc.subjectTectonic evolution-
dc.subjectZircon U-Pb geochronology-
dc.titleGeochronology and geochemistry of meta-mafic dykes in the Quanji Massif, NW China: Paleoproterozoic evolution of the Tarim Craton and implications for the assembly of the Columbia supercontinent-
dc.typeArticle-
dc.identifier.emailSun, M: minsun@hku.hk-
dc.identifier.authoritySun, M=rp00780-
dc.identifier.doi10.1016/j.precamres.2014.04.015-
dc.identifier.scopuseid_2-s2.0-84901228482-
dc.identifier.hkuros252297-
dc.identifier.volume249-
dc.identifier.spage33-
dc.identifier.epage56-
dc.identifier.isiWOS:000339038100003-

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