莎车盆地蒸发岩及盐矿物特征初探  

BRIEF DISCUSSION ON EVAPORITE AND SALT MINERALS CHARACTERISTICS OF SHACHE BASIN

作　　者：曹养同[1] 焦鹏程[1] 宣之强[1] 刘成林[1] 赵宪福[1] 高超[1] 

机构地区：[1]中国地质科学院矿产资源研究所,北京100037

出　　处：《化工矿产地质》2011年第3期137-142,共6页Geology of Chemical Minerals

基　　金：国家"十一五"科技支撑课题"塔里木盆地钾盐大规模成矿条件与找矿靶区预测技术"(2006BAB07B06)资助

摘　　要：莎车盆地喀什皮拉里剖面岩矿扫描电镜及能谱仪分析表明,大量石膏岩中含有石盐、钙芒硝、杂卤石、天青石、白云石及钾镁硫酸盐组合,说明盆地已达到钾镁盐化学沉积阶段,是成钾找钾重要线索,值得研究关注。According to the analysis on Pilalri profile with scanning electron microscope and energy spectrometer, we found that most gypsum rocks have rock salt, glauberite, polyhalite, celestite, dolomite and K-Mg sulfate, all of which show that the basin were coming through the chemical sedimentation phase of abraum salt. It is important for sylvine sedimentation and prospecting.

关 键 词：莎车盆地 喀什皮拉里剖面 石膏与含钾矿物 

分 类 号：P618.13[天文地球—矿床学]