吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (5): 1340-1357.doi: 10.13278/j.cnki.jjuese.20190294
• 整装勘查区矿床成因与成矿作用研究专辑 • 上一篇 下一篇
张连昌1,2,3, 张帮禄1,2,3, 董志国1,2,3, 谢月桥4, 李文君1,2,3, 彭自栋1,2,3, 朱明田1,2,3, 王长乐1,2,3
Zhang Lianchang1,2,3, Zhang Banglu1,2,3, Dong Zhiguo1,2,3, Xie Yueqiao4, Li Wenjun1,2,3, Peng Zidong1,2,3, Zhu Mingtian1,2,3, Wang Changle1,2,3
摘要： 西昆仑北段玛尔坎苏地区探明的大型碳酸锰成矿带，是我国近年最重要的找矿成果之一。该锰矿带构造上属北昆仑晚古生代弧后伸展盆地，其构造动力学背景为古特提斯洋向北俯冲于塔里木地块之下形成的弧盆体系。锰矿体主要发育于晚石炭世喀拉阿特河组含炭泥质灰岩夹薄层灰岩中。矿石中主要金属矿物为菱锰矿（75%~95%），次为软锰矿、硫锰矿及少量黄铁矿等。含锰岩系岩性和岩相学研究表明，玛尔坎苏锰矿带属典型的海相沉积锰矿床，其矿床成因可能与晚古生代半局限盆地沉积和海底热液活动有关。海底热液活动可能为成矿提供了丰富的物质来源。含锰岩系元素和同位素地球化学特征表明，玛尔坎苏锰矿沉淀时的水体环境为常氧条件，而矿层下盘（部分）岩系的岩性及地球化学特征反映其沉积时的水体环境为低氧—贫氧条件。玛尔坎苏锰矿带锰矿石具有负的δ13C值（-23.3‰~-10.0‰），推测有机质导致的还原作用是该锰矿由原生氧化锰在成岩期转化为菱锰矿和形成富锰矿的重要机制。
中图分类号:
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