摘要
钾矿是我国目前紧缺的矿种之一 ,钾矿的寻找对我国有着十分重要的意义。塔里木盆地是我国第三系地层的广泛发育区域 ,有一定的找钾远景 ,尤其是库车、莎车等地区。通过对塔里木盆地 (坳陷 )西部的区域地质概况、成矿条件等的介绍 ,运用地球化学的分析测试手段 ,对塔里木盆地西部采集到的样品作了地球化学分析。论述了该区成盐沉积的地球化学特征 ,并讨论了该区形成钾矿的可能性。
At present, potash deposit is a kind of shortage mineral, so it is significant to find potash deposits. There is extensive foreground of potash deposits in Tarim Basin. because the area is the place which the Tertiary System Stratigraphy lies in, especially in Kuche Basin and Shache Basin.According to the description of geology, the author analyses the samples of the study area by geochemistry analysis methods.What's more the writer illustrates the characters of geochemistry in this area. In the end he puts forward to the deposit probability of potash deposit in this area.
出处
《盐湖研究》
CSCD
2003年第2期35-40,共6页
Journal of Salt Lake Research
基金
国家 30 5项目 (2 0 0 1BA6 0 9A 0 7 16 )
