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Article: Electron microprobe chemical ages of monazite from Qinling Group in the Qinling Orogen: Evidence for Late Pan-African metamorphism?

TitleElectron microprobe chemical ages of monazite from Qinling Group in the Qinling Orogen: Evidence for Late Pan-African metamorphism?
Authors
KeywordsElectron Microprobe Dating
Late Pan-African Thermal Event
Monazite
Qinling Orogen
Issue Date2006
PublisherScience China Press. The Journal's web site is located at http://www.springerlink.com/content/1001-6538/
Citation
Chinese Science Bulletin, 2006, v. 51 n. 21, p. 2645-2650 How to Cite?
AbstractElectron microprobe chemical dating was carried out on monazites enclosed in two generations of mineral paragenesis of St + Ky + Grt and Sil + And + Grt + St, respectively, from the Qinling Group. Two different ages, 520±23 Ma and 435±9 Ma, were obtained from these monazites. This indicates that the Qinling Group experienced a metamorphism during the Early Cambrian, which is probably in response to the Late Pan-African subduction-accretion tectonothermal event. © 2006 Science in China Press.
Persistent Identifierhttp://hdl.handle.net/10722/151200
ISSN
2015 Impact Factor: 1.789
ISI Accession Number ID
References

 

DC FieldValueLanguage
dc.contributor.authorChen, Qen_US
dc.contributor.authorChen, Nen_US
dc.contributor.authorWang, Qen_US
dc.contributor.authorSun, Men_US
dc.contributor.authorWang, Xen_US
dc.contributor.authorLi, Xen_US
dc.contributor.authorShu, Gen_US
dc.date.accessioned2012-06-26T06:18:35Z-
dc.date.available2012-06-26T06:18:35Z-
dc.date.issued2006en_US
dc.identifier.citationChinese Science Bulletin, 2006, v. 51 n. 21, p. 2645-2650en_US
dc.identifier.issn1001-6538en_US
dc.identifier.urihttp://hdl.handle.net/10722/151200-
dc.description.abstractElectron microprobe chemical dating was carried out on monazites enclosed in two generations of mineral paragenesis of St + Ky + Grt and Sil + And + Grt + St, respectively, from the Qinling Group. Two different ages, 520±23 Ma and 435±9 Ma, were obtained from these monazites. This indicates that the Qinling Group experienced a metamorphism during the Early Cambrian, which is probably in response to the Late Pan-African subduction-accretion tectonothermal event. © 2006 Science in China Press.en_US
dc.languageengen_US
dc.publisherScience China Press. The Journal's web site is located at http://www.springerlink.com/content/1001-6538/en_US
dc.relation.ispartofChinese Science Bulletinen_US
dc.subjectElectron Microprobe Datingen_US
dc.subjectLate Pan-African Thermal Eventen_US
dc.subjectMonaziteen_US
dc.subjectQinling Orogenen_US
dc.titleElectron microprobe chemical ages of monazite from Qinling Group in the Qinling Orogen: Evidence for Late Pan-African metamorphism?en_US
dc.typeArticleen_US
dc.identifier.emailSun, M:minsun@hku.hken_US
dc.identifier.authoritySun, M=rp00780en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.doi10.1007/s11434-006-2152-7en_US
dc.identifier.scopuseid_2-s2.0-33751006627en_US
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-33751006627&selection=ref&src=s&origin=recordpageen_US
dc.identifier.volume51en_US
dc.identifier.issue21en_US
dc.identifier.spage2645en_US
dc.identifier.epage2650en_US
dc.identifier.isiWOS:000242914600014-
dc.publisher.placeChinaen_US
dc.identifier.scopusauthoridChen, Q=35478183900en_US
dc.identifier.scopusauthoridChen, N=12796732200en_US
dc.identifier.scopusauthoridWang, Q=14046248000en_US
dc.identifier.scopusauthoridSun, M=25932315800en_US
dc.identifier.scopusauthoridWang, X=7501858663en_US
dc.identifier.scopusauthoridLi, X=23469678400en_US
dc.identifier.scopusauthoridShu, G=14046160500en_US

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