吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (5): 1599-1614.doi: 10.13278/j.cnki.jjuese.20200011
• 整装勘查区矿床成因与成矿作用研究专辑 • 上一篇
熊光强1,2, 刘敏3, 张达1, 王忠4
Xiong Guangqiang1,2, Liu Min3, Zhang Da1, Wang Zhong4
摘要： 内蒙古西乌旗迪彦庙蛇绿岩位于二连浩特—贺根山蛇绿岩带与交其尔—锡林浩特蛇绿岩带一线之间，大地构造位于中亚造山带中段的锡林浩特晚古生代褶皱带。本文主要对其内的辉长岩进行了地球化学及年代学研究。研究结果表明：辉长岩w（SiO2）为45.49%~50.48%，w（Al2O3）为13.31%~17.05%，w（K2O）为0.01%~0.65%，w（Na2O）为0.30%~4.15%，w（CaO）为8.00%~19.54%，w（MgO）为5.22%~10.92%，w（P2O5）为0.03%~0.23%，显示西乌旗迪彦庙蛇绿岩中的辉长岩属于高铝、低钾、低钠的拉斑系列；辉长岩的稀土元素总量低，重稀土元素比轻稀土元素富集，微量元素Nb、Zr、Hf、Ti相对亏损，K、Ta、Sr相对富集；La-ICP-MS锆石U-Pb测年获得辉长岩的年龄为（345.3±2.3）Ma，为早石炭世。综合分析，辉长岩可能为受到俯冲作用产生的流体交代而成，而并非结晶分异作用所致；迪彦庙蛇绿岩形成环境为弧前环境。
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