地质与勘探2012,Vol.48Issue(5):947-958,12.
上扬子区寒武系蒸发岩沉积相及成钾潜力分析
Sedimentary Facies of the Cambrian Evaporites in the Upper Yangtze Region and Their Potash-Forming Potential
摘要
Abstract
The Cambrian period is one of the most important potash-forming eras on the Earth. The Siberian Niepa potash deposit that formed in the late Cambrian is one of the largest potash deposits in the world. India and Pakistan also found potash deposits forming in Late Sinian. In Iran are discov- ered potash deposits in the Cambrian System. Contrast to the potash-forming intensity of other continents, the Cambrian period has become a special pot- ash-fomling age in Asia. Recently, more and more Cambrian evaporite basins have been found in China. This study focuses on presentation of the charac- teristics of the upper Yangtze evaporites, and states that there is more than 200 ,O00 km2 evaporite basins in the upper Yangtze area, and delineates two most favorable areas for potash ( sub-basin of gypsum-halite ) : i.e. the Jiangjin-Luzhou and Jiannan -Pengshui areas. These two areas are good geolog- ic settings for further investigation.关键词
上扬子区/寒武系/膏盐岩聚集区/成盐条件/成钾潜力Key words
upper Yangtze area/Cambrian/favorable areas for potash/geologic setting for salt-forming/potential of potash-forming分类
天文与地球科学引用本文复制引用
王淑丽,郑绵平,焦建..上扬子区寒武系蒸发岩沉积相及成钾潜力分析[J].地质与勘探,2012,48(5):947-958,12.基金项目
中国地质调查局项目(编号:1212010011810)、国家自然科学重点基金项目(编号:U0833601)、重点实验室开放基金项目(编号:ZS1113)联合资助. ()