探索中国陆块找钾——中国东特提斯域成钾作用及模式  

RESEARCH ON POTASH EXPLORATION AT CHINA LAND MASS ——POTASH ALTERATION AND PATTERN OF EASTERN TETHYS OCEAN,CHINA

作　　者：刘成林[1] 宣之强 曹养同[1] 王立成[1] 王春连[1] 赵艳军[1] 张华[1] 

机构地区：[1]中国地质科学院矿产资源研究所,北京100037 [2]中化矿山总局地质研究院,河北涿州072754

出　　处：《化工矿产地质》2015年第4期193-197,共5页Geology of Chemical Minerals

基　　金：国家重点基础研究发展计划(973)"中国陆块海相成钾规律及预测研究"【2011CB403 000】项目研究成果

摘　　要：中国陆块海相成钾规律及预测(973)课题五年硏究,完成构建我国海相盆地钾盐成矿理论及"模式"构建。"中国东特提斯域成钾作用及模式"从中国海相蒸发岩盆地成盐聚钾探索中,得出:气侯、物源及构造在时间和空间上"三位一体"耦合作用成钾理论,对东特提斯域成钾提出了"多级盆地"及"深源补给"等成钾模式,为中国陆块找钾提供了理论依据。The five-year topic on regulation and prediction of marine facies potash alteration （973） had gave us the potash formation theory and the pattern construction of marine facies potash. Potash alteration and pattern of Eastern Tethys Ocean in China found the trinity catenative potash alteration theory for climate and material resources as well as the construction in time and space, at the same time, the potash formation pattern of multilevel basin and deep focus supply had also been brought forward which gave the theory foudation for potash exploration in China land mass.

关 键 词：中国陆块 东特提斯域 成钾作用 找钾模式 

分 类 号：P619.211[天文地球—矿床学]