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阿尔金铅、钕、锶、氩、氧同位素研究及其早期演化
引用本文:车自成,刘良,孙勇.阿尔金铅、钕、锶、氩、氧同位素研究及其早期演化[J].地球学报,1995,16(3):334-337.
作者姓名:车自成  刘良  孙勇
作者单位:西北大学地质系;西北大学地质系;西北大学地质系
摘    要:根据铅、钕、锶、氩、氧等同位素体系及其年代学研究,阿尔金在其早期演化阶段中存在2790—2590、1883—1704、575和470—420Ma4个构造热事件,各自具有不同的性质和时代意义。

关 键 词:阿尔金  铅、钕、锶、氩、氧同位素体系  构造演化

U-Pb,Sm-Nd,Rb-Sr,(40)Ar/(39)Ar and (18)O/(16)O LsotopicStudies for Early Evolution of the Structural Belt in Altun Area
CHE Zi-cheng,LIU Liang and SUN Yong.U-Pb,Sm-Nd,Rb-Sr,(40)Ar/(39)Ar and (18)O/(16)O LsotopicStudies for Early Evolution of the Structural Belt in Altun Area[J].Acta Geoscientia Sinica,1995,16(3):334-337.
Authors:CHE Zi-cheng  LIU Liang and SUN Yong
Institution:Department of Geology Northvest University, Xi'an;Department of Geology Northvest University, Xi'an;Department of Geology Northvest University, Xi'an
Abstract:Existing four tectonic events for early evolution of the Altun structural belt,the age is separat-ly 2790 2590, 1883 1704,575 and 470 420Ma. This conclution results from U-Pb,Sm-Nd,Rb-Sr,(40)Ar/(39)Ar,(18)O/(16)O iSotopic system studies. Four data respectively represent basement forma-tion,cratonization,accretion and collision of the plate located Altun mountain in.
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