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新桥硫-多金属矿床含硫磁铁矿体地质特征及成因探讨
引用本文:陈彬.新桥硫-多金属矿床含硫磁铁矿体地质特征及成因探讨[J].化工矿产地质,2003,25(3):173-178.
作者姓名:陈彬
作者单位:铜陵化工集团新桥矿业公司
摘    要:通过对新桥硫-多金属矿床含硫磁铁矿矿体赋存空间、构造环境、岩矿组合、围岩蚀变等宏观地质特征的研究,并结合微量元素,硫、铅、氢、氧同位素、矿物包体测温等资料综合分析认为:本区成矿物质来源为中深相幔源岩浆或同熔岩浆,进而研究矿床含硫磁铁矿体应属高温热液交代-后期热液叠加改造成因类型。

关 键 词:地质特征  物源  成矿阶段  成矿机理
文章编号:1006-5296(2003)03-0173-06
修稿时间:2003年3月21日

GEOLOGICAL FEATURES AND GENETIC STUDY OF THE CONTAINING SULFUR-MAGNATITE OREBODY OF XIN QIAO DEPOSIT
Chen Bin.GEOLOGICAL FEATURES AND GENETIC STUDY OF THE CONTAINING SULFUR-MAGNATITE OREBODY OF XIN QIAO DEPOSIT[J].Geology of Chemical Minerals,2003,25(3):173-178.
Authors:Chen Bin
Institution:Xin Qiao mining company of TCIGCL
Abstract:According to the features of the orebodies locations and associations of rocks and minerals ,and alterations of the wall rocks. The metallogenic geological conditions and process is investigated from field survey and analyses of trace elements and isotopes . It is proposed that the containing sulfur - magnetite orebody of this deposit belongs to the genetic type of the high temperature hydrothermal - alternate and hydrothermal superimposition.
Keywords:containing sulfur-magnetite orebody  Geological features  Genesis  Xin Qiao  
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