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贵州五指山背斜纳雍枝铅锌矿地质特征及找矿前景分析
引用本文:吴先彪,朱尤清,廖树衡,锁瑞强. 贵州五指山背斜纳雍枝铅锌矿地质特征及找矿前景分析[J]. 地质与资源, 2013, 22(6): 493-498
作者姓名:吴先彪  朱尤清  廖树衡  锁瑞强
作者单位:贵州省有色金属和核工业地质勘查局一总队, 贵州 清镇 551400
摘    要:纳雍枝铅锌矿床位于五指山背斜北东部,是五指山矿集区的组成部分.区内铅锌矿体产于清虚洞组的白云岩中,自下而上共划分为9个矿体层,属沉积型铅锌矿床.矿石类型为碳酸盐岩型铅锌矿石.五指山地区位于紫云-垭都深大断裂的北东侧,南东侧有安顺-凯里深断裂,这些深断裂是纳雍枝矿床深部物质来源的前提,次一级的构造为矿床的形成提供了矿质流动的通道.五指山背斜Pb、Zn综合异常明显的部位,异常与区内构造较吻合,与矿床(点)展布方向一致.该矿床与典型密西西比河谷铅锌矿床具有较高的可比性.通过对纳雍枝铅锌矿床地质特征的总结及分析,认为五指山地区的找矿前景十分广阔.

关 键 词:纳雍枝铅锌矿  地质特征  找矿前景  五指山  贵州省
收稿时间:2012-06-11

GEOLOGICAL CHARACTERISTICS AND PROSPECTING ANALYSIS OF THE NAYONGZHI LEAD-ZINC DEPOSIT IN WUZHISHAN ANTICLINE,NORTHWESTERN GUIZHOU
WU Xian-biaoNo.,Team,Guizhou Bureau of Geological Exploration for Nonferrous Metal and Nuclear Industry,Qingzhen,Guizhou Province,China ZHU You-qingNo.,Team,Guizhou Bureau of Geological Exploration for Nonferrous Metal and Nuclear Industry,Qingzhen,Guizhou Province,China LIAO Shu-hengNo.,Team,Guizhou Bureau of Geological Exploration for Nonferrous Metal and Nuclear Industry,Qingzhen,Guizhou Province,China SUO Rui-qiang. GEOLOGICAL CHARACTERISTICS AND PROSPECTING ANALYSIS OF THE NAYONGZHI LEAD-ZINC DEPOSIT IN WUZHISHAN ANTICLINE,NORTHWESTERN GUIZHOU[J]. Geology and Resources, 2013, 22(6): 493-498
Authors:WU Xian-biaoNo.  Team  Guizhou Bureau of Geological Exploration for Nonferrous Metal  Nuclear Industry  Qingzhen  Guizhou Province  China ZHU You-qingNo.  Team  Guizhou Bureau of Geological Exploration for Nonferrous Metal  Nuclear Industry  Qingzhen  Guizhou Province  China LIAO Shu-hengNo.  Team  Guizhou Bureau of Geological Exploration for Nonferrous Metal  Nuclear Industry  Qingzhen  Guizhou Province  China SUO Rui-qiang
Affiliation:No. 1 Team, Guizhou Bureau of Geological Exploration for Nonferrous Metal and Nuclear Industry, Qingzhen 551400, Guizhou Province, China
Abstract:The Nayongzhi Pb-Zn deposit,situated in the northeast of Wuzhishan anticline,is a component of the Wuzhishan ore-concentrating zone.The orebodies occur in the dolostone of Cambrian Qingxudong formation,consisting of nine ore layers.The ores belong to carbonate rock type.The Ziyun-Yadu deep fault in the southwest and Anshun-Kaili deep fault in the southeast of the region are the prerequisites for the material source of the deposit.The secondary structures provide flow channels for ore fluid.The comprehensive Pb-Zn anomalies coincide to the regional structures,as well as the distribution of ore deposits (occurrences).The Nayongzhi Pb-Zn deposit is much comparable to the Mississippi Valley Pb-Zn deposit.The geological characteristics of Nayongzhi Pb-Zn deposit show a great prospect of exploration in Wuzhishan region.
Keywords:Nayongzhi Pb-Zn deposit  geological characteristics  metallogenic prospect  Wuzhishan  Guizhou Province
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