LA-ICPMS Zircon U-Pb Age of the Zhongchaye Vermiculite Deposit in Laiwu,Shandong Province  

作　　者：LI Jie LI Shiyong SU Xuliang SONG Mingchun 

机构地区：[1]Hebei Key Laboratory of Strategic Critical Mineral Resources,Hebei GEO University,Shijiazhuang 050031,China [2]School of Earth Sciences,Hebei GEO University,Shijiazhuang 050031,China [3]Center of Deep Sea Research,Institute of Oceanology,Chinese Academy of Sciences,Qingdao,Shandong 266071,China [4]The Geophysics and Geochemistry Research Institute in Shandong Province,Jinan 250013,China [5]Qingdao Geo-engineering Investigation Institute,Qingdao,Shandong 266000,China [6]Shandong Provincial No.6 Exploration Institute of Geology and Mineral Resources,Weihai,Shandong 264209,China

出　　处：《Acta Geologica Sinica(English Edition)》2020年第5期1721-1723,共3页地质学报（英文版）

基　　金：funded by Natural Science Foundation of Hebei province(D2020403061);Taishan Scholar Program of Shandong(grant No.ts201511076);National Research and Development Program of China(2016YFC0600408);Key Research and Development Project of Shandong Province(2017CXGC1604);Geological Exploration Project of Shandong Province(202017);Opening Fondation of Key Laboratory of Regional Geology and Mineralization,Hebei GEO University(HGU-RGM2017)。

摘　　要：Objective The Zhongchaye vermiculite deposit is located north of Laiwu.Tectonically,it belongs to the Luxi Block,west of the Tan-Lu fault zone(Fig.1a).The crystalline basement of this area consists of the Neoarchean Taishan Group and Paleoproterozoic Granitoid.The overlying strata are mainly Paleozoic carbonate rocks,Mesozoic clastic rocks。

关 键 词：STRATA belongs CARBONATE 

分 类 号：P597.3[天文地球—地球化学] P619.2[天文地球—地质学]