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《Acta Sedimentologica Sinica》 2003-04
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Tectonic Setting and Provenance of Source Rock for Sedimentary Rocks in Lanping Mesozoic-Cenozoic Basin:evidences from geochemistry of sandstones

LI Zhi ming 1,2 LIU Jia jun 3 HU Rui zhong 1 LIU Yu ping 1 LI Chao yang 1 HE Ming qin 1 1(The Open Laboratory of Ore Deposit Geochemistry, Chinese Academy of Sciences, Guiyang 550002) 2(The Postgraduate Institute, Chinese Academy of Sciences, Beijing 100039) 3(China University of Geosciences, Beijing 100083)  
The geochemical compositions of sandstones in sedimentary basin are controlled by the tectonic setting of source rock, and it is, therefore, possible to discriminate the tectonic setting of source rock area and provenance of source rock by studying the geochemical compositions of sandstones. The major compositions, rare earth elements and trace elements of Mesozoic Cenozoic sandstones in Lanping Basin are studied in this paper, and which reveals that the tectonic settings of source rock area for Mesozoic Cenozoic sedimentary rocks in in Lanping Basin, belong to passive continental margin and continental island arc. Combined with the data of sedimentary facies and palaeogeography, it is referred that the east area of basin is mainly located at tectonic setting of passive continental margin before Mesozoic , whereas the west area of basin may be at continental island arc. This is compatible with the results of regional geological studied data. The primary materials of sedimentary rocks should come from the upper continental crust, and are mainly composed of felsic rocks, mixed with few andesitic rocks and old sediment components. Therefore , Lanping Mesozoic Cenozoic Basin is the typical continental type basin. This provides strong geochemical evidences for correctly understanding the evolution of the old Tethys and the basin range transition.
【Fund】: 国家重点基础研究发展规划项目(编号 :G1 9990 4 32 0 8)资助
【CateGory Index】: P544.4
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