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Article: Zircon U-Pb ages of the fuping complex and their implications: Some comments on the geochronological study of the precambrian high-grade metamorphic terranes

TitleZircon U-Pb ages of the fuping complex and their implications: Some comments on the geochronological study of the precambrian high-grade metamorphic terranes
Authors
KeywordsFuping Complex
Icpms-Lp
Shrimp
Tims
Zircon U-Pb Age
Issue Date2001
PublisherChinese Academy of Sciences, Institute of Geology and Geophysics. The Journal's web site is located at http://www.ysxb.ac.cn/ysxb/ch/index.aspx
Citation
Acta Petrologica Sinica, 2001, v. 17 n. 1, p. 145-156 How to Cite?
AbstractThree zircon U-Pb age dating methods have been applied for the Fuping Complex, i.e. Thermal Ionization Mass Spectrometry (TIMS), Sensitive High Resolution Ion MicrProbe (SHRIMP) and Inductively Coupled Plasma Mass Spectrometry - Laser Probe (ICPMS-LP). Based on these results it is suggested that the Fuping Complex is mainly made up of 2. 51 Ga TTG gneisses; a small amount of 2.7 Ga hornblende gneisses were developed which may represent the fragments of old continental materials. One magmatic event of 2.05 Ga was confirmed in the Fuping area. The Wanzi supracrustal rocks were possibly deposited between 2.5 and 2.1 Ga. The characteristics of the three U-Pb dating techniques and their applications on the geochronological study of the Precambrian high-grade metamorphic rocks were also discussed. It is emphasized the significance of the study on the internal structures, chemical characteristics on zircon for its U-Pb geochronology.
Persistent Identifierhttp://hdl.handle.net/10722/151054
ISSN
2015 Impact Factor: 1.234
2015 SCImago Journal Rankings: 0.892
References

 

DC FieldValueLanguage
dc.contributor.authorSun, Men_US
dc.contributor.authorGuan, Hen_US
dc.date.accessioned2012-06-26T06:16:34Z-
dc.date.available2012-06-26T06:16:34Z-
dc.date.issued2001en_US
dc.identifier.citationActa Petrologica Sinica, 2001, v. 17 n. 1, p. 145-156en_US
dc.identifier.issn1000-0569en_US
dc.identifier.urihttp://hdl.handle.net/10722/151054-
dc.description.abstractThree zircon U-Pb age dating methods have been applied for the Fuping Complex, i.e. Thermal Ionization Mass Spectrometry (TIMS), Sensitive High Resolution Ion MicrProbe (SHRIMP) and Inductively Coupled Plasma Mass Spectrometry - Laser Probe (ICPMS-LP). Based on these results it is suggested that the Fuping Complex is mainly made up of 2. 51 Ga TTG gneisses; a small amount of 2.7 Ga hornblende gneisses were developed which may represent the fragments of old continental materials. One magmatic event of 2.05 Ga was confirmed in the Fuping area. The Wanzi supracrustal rocks were possibly deposited between 2.5 and 2.1 Ga. The characteristics of the three U-Pb dating techniques and their applications on the geochronological study of the Precambrian high-grade metamorphic rocks were also discussed. It is emphasized the significance of the study on the internal structures, chemical characteristics on zircon for its U-Pb geochronology.en_US
dc.languageengen_US
dc.publisherChinese Academy of Sciences, Institute of Geology and Geophysics. The Journal's web site is located at http://www.ysxb.ac.cn/ysxb/ch/index.aspxen_US
dc.relation.ispartofActa Petrologica Sinicaen_US
dc.subjectFuping Complexen_US
dc.subjectIcpms-Lpen_US
dc.subjectShrimpen_US
dc.subjectTimsen_US
dc.subjectZircon U-Pb Ageen_US
dc.titleZircon U-Pb ages of the fuping complex and their implications: Some comments on the geochronological study of the precambrian high-grade metamorphic terranesen_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.scopuseid_2-s2.0-0034920471en_US
dc.identifier.hkuros58008-
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-0034920471&selection=ref&src=s&origin=recordpageen_US
dc.identifier.volume17en_US
dc.identifier.issue1en_US
dc.identifier.spage145en_US
dc.identifier.epage156en_US
dc.publisher.placeChinaen_US
dc.identifier.scopusauthoridSun, M=25932315800en_US
dc.identifier.scopusauthoridGuan, H=36901914400en_US

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