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宁夏中宁茶梁子铁钴矿床成矿地质特征
引用本文:刘志坚,侯明才,王泽晶,等.宁夏中宁茶梁子铁钴矿床成矿地质特征[J].地质学刊,2013,37(4):642-646.
作者姓名:刘志坚  侯明才  王泽晶  
作者单位:成都理工大学沉积地质研究院
基金项目:中国地质调查局地质调查项目(1212011085087)
摘    要:通过对茶梁子矿区的地质背景、矿体特征、矿石特征及岩石地球化学特征进行综合研究,初步探讨了矿床的成因。认为矿体是由含硫质的低温热液携带矿质运移到断裂构造的有利部位沉淀而形成的。同时在表生环境下,原生矿体经过后期的次生改造作用后,形成了富含铁、锰氧化物的土状矿石,并且以较为富集的铁、锰氧化物作为寻找钴的直接标志。

关 键 词:铁钻矿  成矿地质特征  地球化学特征  茶梁子  宁夏中宁
收稿时间:2013/2/25 0:00:00
修稿时间:4/1/2013 12:00:00 AM

Metallogenic geological characteristics of Chaliangzi Fe-Co deposit in Zhongning in Ningxia
LIU Zhi-jian.Metallogenic geological characteristics of Chaliangzi Fe-Co deposit in Zhongning in Ningxia[J].Jiangsu Geology,2013,37(4):642-646.
Authors:LIU Zhi-jian
Institution:1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China; 2. Geological Survey Institute of Ningxia Hui Autonomous Region, Yinchuan 750021, China)
Abstract:Based on analyses of geological background, ore body features and petro-geochemistry features, the authors preliminary discussed the genesis of ore deposits in Chaliangzi ore district. The formation of ore bodies were related to sulfur-rich epithermal fluid. The fluid carried minerals and transported to the vantage point of fault zone, and then the minerals were deposited. In the superficial environment, primary ore body change into earthy ore that was rich in iron manganese oxide by secondary reformation.The rich iron manganese oxide could be the indicators for exploring cobalt ore.
Keywords:Fe-Co deposit  Metallogenic geological properties  Geochemical properties  Chaliangzi  Zhongning  Ningxia
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