Aneu新疆富蕴县扎河坝地区不同矿床物探异常识别标志浅析  

Aneu Xinjiang Fuyun County Bar geophysical anomaly identification mark different deposit area of dam

作　　者：高万杰 代晓龙 冉座 

机构地区：[1]新疆维吾尔自治区地质矿产开发局物化探大队,新疆昌吉831100

出　　处：《世界有色金属》2017年第23期249-250,共2页World Nonferrous Metals

摘　　要：研究区位于哈萨克斯坦-准葛尔板块北缘,查尔斯克-乔夏哈拉缝合线的南侧,是西伯利亚板块和准噶尔板块斜向碰撞对接的构造部位,额尔齐斯、二台两大断裂在此交汇。区内经历多期次构造活动及不同应力场的作用,地质构造比较复杂,形成多种构造单元的交汇,地层与岩浆岩分布主要受主干深断裂控制,岩浆活动频繁,成矿作用明显,是一个较好的矿化密集区。The research area is located on the southern side of the Kazakhstan-Junggar plate,on the south side of the Charles Ke Qiao Xia Hara suture.It is the structural part of oblique collision between Siberia plate and Junggar plate.Earl Keith and two two major faults meet here.Multi tectonic activities and different stress field in the region,the geological structure is complex,the formation of various intersection tectonic units,stratum and magmatite distribution is mainly controlled by the main control of deep faults,frequent magmatic activities,the mineralization obviously,is a good mineralization concentrated area.

关 键 词：扎河坝 构造 断裂 褶皱 断层接触 蛇绿岩套 构造蚀变 火山热液 矿体 隐伏 极化率 电阻率 物性特征 

分 类 号：P542.3[天文地球—构造地质学]