File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

Article: Geochronology of the volcanic rocks in the Lu-Zong basin and its significance

TitleGeochronology of the volcanic rocks in the Lu-Zong basin and its significance
Authors
KeywordsGeochronologic Age
Lu-Zong Basin
Volcanic Rocks
Zircon La-Icp Ms Dating
Issue Date2008
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, 2008, v. 51 n. 10, p. 1470-1482 How to Cite?
AbstractThe Lu-Zong (Lujiang-Zongyang) basin is one of the most important volcanic basins in the middle and lower reaches of the Yangtze River area, China. It comprises four shoshonitic volcanic units, which are, in an ascending order, the Longmenyuan, Zhuanqiao, Shuangmiao and Fushan Groups. The LA-ICP MS U-Pb zircon ages of the four units are: 134.8±1.8 Ma for the Longmenyuan Group, 134.1±1.6 Ma for the Zhuanqiao Group, 130.5±0.8 Ma for the Shuangmiao Group, and 127.1±1.2 Ma for the Fushan Group. The results indicate that all volcanic rocks in the Lu-Zong basin were formed in the Early Cretaceous from about 135 Ma to 127 Ma, lasting 8-10 Ma. There were no Jurassic volcanic activities in all the volcanic basins including the Lu-Zong basin in the middle and lower reaches of the Yangtze River area. This work has provided new chronological results for the further study and understanding of the tectonic, magmatic and metallogenic processes of eastern China in the Mesozoic. © Science in China Press and Springer-Verlag GmbH 2008.
Persistent Identifierhttp://hdl.handle.net/10722/151258
ISSN
2011 Impact Factor: 1.588
ISI Accession Number ID
Funding AgencyGrant Number
National Basic Research Program of China2007CB411405
National Natural Science Foundation of China40672062
Specialized Research Fund20050359013
Scientific Research Project of CODES
Centre of Excellence in Ore Deposits
University of TasmaniaCODES2006N2.3
Anhui Public Geologic Projects2005-48
2007-1
Anhui Provincial Science Foundation for Distinguished Young Scholars08040106907
04045063
Funding Information:

Supported by the National Basic Research Program of China (Grant No. 2007CB411405), the National Natural Science Foundation of China (Grant No. 40672062), the Specialized Research Fund for the Doctoral Program of Higher Education (Grant No. 20050359013), the Scientific Research Project of CODES, Centre of Excellence in Ore Deposits, University of Tasmania (Grant No. CODES2006N2.3), the Anhui Public Geologic Projects (Grant No. 2005-48, 2007-1), and the Anhui Provincial Science Foundation for Distinguished Young Scholars (Grant Nos. 08040106907, 04045063)

References

 

DC FieldValueLanguage
dc.contributor.authorZhou, TFen_US
dc.contributor.authorFan, Yen_US
dc.contributor.authorYuan, Fen_US
dc.contributor.authorLu, SMen_US
dc.contributor.authorShang, SGen_US
dc.contributor.authorCooke, Den_US
dc.contributor.authorMeffre, Sen_US
dc.contributor.authorZhao, GCen_US
dc.date.accessioned2012-06-26T06:19:30Z-
dc.date.available2012-06-26T06:19:30Z-
dc.date.issued2008en_US
dc.identifier.citationScience In China, Series D: Earth Sciences, 2008, v. 51 n. 10, p. 1470-1482en_US
dc.identifier.issn1006-9313en_US
dc.identifier.urihttp://hdl.handle.net/10722/151258-
dc.description.abstractThe Lu-Zong (Lujiang-Zongyang) basin is one of the most important volcanic basins in the middle and lower reaches of the Yangtze River area, China. It comprises four shoshonitic volcanic units, which are, in an ascending order, the Longmenyuan, Zhuanqiao, Shuangmiao and Fushan Groups. The LA-ICP MS U-Pb zircon ages of the four units are: 134.8±1.8 Ma for the Longmenyuan Group, 134.1±1.6 Ma for the Zhuanqiao Group, 130.5±0.8 Ma for the Shuangmiao Group, and 127.1±1.2 Ma for the Fushan Group. The results indicate that all volcanic rocks in the Lu-Zong basin were formed in the Early Cretaceous from about 135 Ma to 127 Ma, lasting 8-10 Ma. There were no Jurassic volcanic activities in all the volcanic basins including the Lu-Zong basin in the middle and lower reaches of the Yangtze River area. This work has provided new chronological results for the further study and understanding of the tectonic, magmatic and metallogenic processes of eastern China in the Mesozoic. © Science in China Press and Springer-Verlag GmbH 2008.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.subjectGeochronologic Ageen_US
dc.subjectLu-Zong Basinen_US
dc.subjectVolcanic Rocksen_US
dc.subjectZircon La-Icp Ms Datingen_US
dc.titleGeochronology of the volcanic rocks in the Lu-Zong basin and its significanceen_US
dc.typeArticleen_US
dc.identifier.emailZhou, T: tfzhou@hfut.edu.cnen_US
dc.identifier.emailZhao, G: gzhao@hkucc.hku.hk-
dc.identifier.authorityZhao, GC=rp00842en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.doi10.1007/s11430-008-0111-7en_US
dc.identifier.scopuseid_2-s2.0-52249121799en_US
dc.identifier.hkuros154945-
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-52249121799&selection=ref&src=s&origin=recordpageen_US
dc.identifier.volume51en_US
dc.identifier.issue10en_US
dc.identifier.spage1470en_US
dc.identifier.epage1482en_US
dc.identifier.isiWOS:000259790100011-
dc.publisher.placeChinaen_US
dc.identifier.scopusauthoridZhou, TF=7402989472en_US
dc.identifier.scopusauthoridFan, Y=35794447800en_US
dc.identifier.scopusauthoridYuan, F=35333422400en_US
dc.identifier.scopusauthoridLu, SM=13612431500en_US
dc.identifier.scopusauthoridShang, SG=24833635900en_US
dc.identifier.scopusauthoridCooke, D=7202107225en_US
dc.identifier.scopusauthoridMeffre, S=6602112080en_US
dc.identifier.scopusauthoridZhao, GC=7403296321en_US

Export via OAI-PMH Interface in XML Formats


OR


Export to Other Non-XML Formats