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Zircon U-Pb Ages of the Muchang Alkali Granites in Zhenkang Block, Western Yunnan: Implication for the Time Limit on Tectono-Magmatic Activities 被引量:4
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作者 YANG Fucheng LI Wenchang +4 位作者 LIU Xuelong WANG Shuaishuai YANG Yunkai GU Youwei LUO Ying 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2019年第4期1152-1153,共2页
Objective The Luziyuan super-large Pb-Zn-Fe polymetallic ore district is located in the southern section of the Baoshan-Zhenkang block,which is an important part of the Pb-Zn-Cu-Fe-Sn-Au polymetallic metallogenic belt... Objective The Luziyuan super-large Pb-Zn-Fe polymetallic ore district is located in the southern section of the Baoshan-Zhenkang block,which is an important part of the Pb-Zn-Cu-Fe-Sn-Au polymetallic metallogenic belt,SW China. 展开更多
关键词 PB ZN BLOCK
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The Late Cretaceous Crustal Magmatism of the Geza Arc Metallogenic Belt in Yunnan Province,and Zircon Ages and Hf Isotopic Evidence of the Porphyry Cu-Mo Mineralization 被引量:2
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作者 YANG Fucheng LI Wenchang +1 位作者 LIU Xuelong WANG Shuaishuai 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2017年第1期355-356,共2页
Objective The Geza arc in Yunnan Province,located in the southern Yidun arc,is an important part of the Sanjiang tectonic-magmatic belts in southwestern China and is a newly discovered copper polymetallic ore-concentr... Objective The Geza arc in Yunnan Province,located in the southern Yidun arc,is an important part of the Sanjiang tectonic-magmatic belts in southwestern China and is a newly discovered copper polymetallic ore-concentrating district.Recent studies show that the newly discovered Yanshanian porphyry Cu-Mo polymetallic mineralization superimposed in the Indosinian porphyry copper belt in this area. 展开更多
关键词 HF The Late Cretaceous Crustal Magmatism of the Geza Arc Metallogenic Belt in Yunnan Province and Zircon Ages and Hf Isotopic Evidence of the Porphyry Cu-Mo Mineralization MO Cu
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Applicability of large-ion lithophile and high field strength element basalt discrimination diagrams 被引量:2
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作者 X.L.Liu Q.Zhang +11 位作者 W.C.Li F.C.Yang Y.Zhao Z.Li S.T.Jiao J.R.Wang N.Zhang S.S.Wang W.F.Chen Z.J.Pan J.Yang X.L.Du 《International Journal of Digital Earth》 SCIE EI 2018年第7期752-760,共9页
Basalt discriminant diagrams have been used to identify the tectonic setting of basaltic magmatism since the 1970s and have played an important role in reconstructing paleotectonic environments.However,the significant... Basalt discriminant diagrams have been used to identify the tectonic setting of basaltic magmatism since the 1970s and have played an important role in reconstructing paleotectonic environments.However,the significant increase in the availability of geochemical data has led to a reassessment of these diagrams,suggesting that some of the tectonic settings indicated by these diagrams are not accurate.Here,we use a database of global ocean island basalt(OIB),mid-ocean ridge basalt(MORB),and island arc basalt(IAB)geochemistry to propose a series of new tectonic discriminant diagrams based on the ratios of large-ion lithophile elements(LILEs)to high field strength elements(HFSEs).These new diagrams indicate that the LILE can be used to differentiate OIB,MORB,and IAB samples,meaning that LILE/HFSE ratios can discriminate between these basalts that form in different tectonic settings.Our new diagrams can correctly assign samples to OIB,MORB,and IAB categories more than 85%of the time,with the discrimination between OIB and MORB having an accuracy of slightly less than 85%. 展开更多
关键词 BASALT LILE HFSE discrimination diagram geochemistry
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