湖北省安陆市张家湾钒钼矿床地质特征、成因探讨及找矿方向  

Geological Characteristics of the Zhangjiawan Vanadium Molybdenum Deposit,Genesis and Prospecting Direction in Anlu City in Hubei Province

作　　者：陈炜[1,2] 周文平[2] 周仁君[2] 王彤[2] 贺慧艳[2] 宋志强[2] 方明[2] 

机构地区：[1]中国地质大学地球科学学院,湖北武汉430074 [2]湖北省鄂东北地质大队,湖北孝感432100

出　　处：《资源环境与工程》2014年第2期126-131,共6页Resources Environment & Engineering

基　　金：湖北省财政部门预算专项资金[2010]18号

摘　　要：张家湾矿区位于襄樊—广济断裂北东边缘的云林寺复式褶皱中部的张家湾倒转向斜两翼;张家湾钒钼矿床严格受控于早寒武世杨家堡组和庄子沟组中的一套黑色硅质岩及黏土岩等,为海底热水(喷气)和生物成矿相互作用沉积型层控矿床,寒武纪地层、黑色岩性、V-Mo综合异常是其特有找矿标志和找矿方向。Zhangjiawan mine is located in the middle of Yunlin temple complex fold in North East edge of Xiangfan Guangji fault. Zhangjiawan vanadium molybdenum deposit is strictly controlled by the Early Cambrian of Yangjiabu group and the Chuang-tzu formation in a black chert and clay rocks, the submarine hot water .jet sedimentary deposits have pros- pecting criteria and prospecting direction about strata, lithology and V-Mo anomaly.

关 键 词：矿床地质特征 矿床成因 找矿方向 张家湾钒钼 湖北安陆市 

分 类 号：P618.61[天文地球—矿床学] P618.65[天文地球—地质学]