新疆西昆仑玛尔坎苏锰矿带成矿地质特征及找矿方向  

Metallogenic Geological Characteristics and Prospecting Direction of Maerkansu Manganese Ore Belt in West Kunlun,Xinjiang

作　　者：高永宝[1] 滕家欣 陈登辉[1] 隋清霖[1] 

机构地区：[1]国土资源部岩浆作用成矿与找矿重点实验室,中国地质调查局西安地质调查中心,陕西西安710054

出　　处：《西北地质》2017年第1期261-269,共9页Northwestern Geology

基　　金：陕西省科学技术研究发展计划项目“东昆仑祁漫塔格地区中生代中酸性侵入岩浆活动与成矿作用”(2015KJXX-71);中国地质调查局地质调查项目“秦祁昆造山系地质构造演化与成矿规律研究”(1212011121088);“南疆工程及西昆仑成矿带矿产勘查部署与综合研究”(12120115019501);“西昆仑铁铅锌资源基地调查与勘查示范”(DD20160015);“中国矿产地质与成矿规律综合集成和服务”(DD20160346),中国地质调查局青年地质英才计划(2013)联合资助

摘　　要：西昆仑玛尔坎苏地区晚石炭世优质锰矿找矿取得重大突破,锰矿带层位稳定,厚度较大,品位富,属于典型的海相沉积型锰矿床。笔者通过对成矿地质背景及典型矿床成矿地质特征进行研究,分析控矿地质条件,提出含碳泥晶灰岩、背斜构造、断裂构造、遥感及地球物理等找矿标志,认为玛尔坎苏锰矿带外围及深部找矿潜力巨大,应加强奥尔托喀讷什锰矿床南翼、苏萨尔布拉克、博托彦、托库孜布拉克等的锰矿找矿工作;应重视矿田构造的研究,拓展深部找矿空间;塔里木西缘及北缘石炭系锰矿找矿工作需进一步重视。A major breakthrough for high quality manganese ore prospecting was made in Maerkansu area, west Kunlun. The manganese ore belt in Maerkansu area is stable with large thickness and rich grade, and the manganese deposits belong to a typical marine sedimentary manganese deposit. In this paper, we study the geological background of mineralization, the geological characteristics of typical deposits and ore-controlling geological conditions. The ore-prospecting criterias were proposed, which include the Carbonaceous micrite, anticline structure, fracture structure, remote sensing and geophysics. It is indicated that there is huge prospecting potential of Maerkansu manganese ore belt. Prospecting work should be reinforced in the south wing of Aoertuokane deposit, Suesalburak, Botuoyan and Tuokuzibulake, and so on. Meanwhile, more attentions should be paid to the study of ore field structure to develop ore prospecting in depth. Prospecting work of Carboniferous manganese deposits in the western and northen margin of Tar-im needs further attentions.

关 键 词：成矿地质特征 找矿标志 找矿方向 玛尔坎苏 西昆仑 

分 类 号：P618.32[天文地球—矿床学]