A Cretaceous Desert-Playa Sedimentary System Controlled the Potash Formation in the Simao Basin  

作　　者：WU Chihua LIU Chenglin SHEN Lijian WANG Jiuyi ZHANG Hua 

机构地区：[1]School of Marine Sciences,Sun Yat-sen University [2]Guangdong Provincial Key Laboratory of Marine Resources and Coastal Engineering [3]MLR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resources,Chinese Academy of Geological Sciences

出　　处：《Acta Geologica Sinica(English Edition)》2017年第3期1143-1144,共2页地质学报（英文版）

基　　金：supported by the Chinese National Key Project for Basic Research(grant No. 2011CB403007);the National Natural Science Foundation of China(grant No.41602127)

摘　　要：Objective The Simao Basin in Yunnan Province has developed Cretaceous evaporite-bearing clastic deposits, including the Mangang and Mengyejing Formations which were originally interpreted as fluvial and lacustrine deposits. The Mangang Fm. composed of well-rounded quartz sandstones, were commonly considered as the bottom part of the Mengyejing salt series. Dttring last decades,Objective The Simao Basin in Yunnan Province has developed Cretaceous evaporite-bearing clastic deposits, including the Mangang and Mengyejing Formations which were originally interpreted as fluvial and lacustrine deposits. The Mangang Fm. composed of well-rounded quartz sandstones, were commonly considered as the bottom part of the Mengyejing salt series. Dttring last decades,

关 键 词：A Cretaceous Desert-Playa Sedimentary System Controlled the Potash Formation in the Simao Basin is for as were that of 

分 类 号：P534.53[天文地球—古生物学与地层学] P619.211[天文地球—地质学]