矿床地质:2016,Vol.>>Issue(3):524-538

河南省嵩县槐树坪金矿床地质、同位素地球化学特征与成矿作用
中国地质大学, 北京 100083;五矿勘查开发有限公司, 北京 100010,五矿勘查开发有限公司, 北京 100010,中国地质大学地质过程 与矿产资源国家重点实验室, 北京 100083,五矿勘查开发有限公司, 北京 100010,五矿勘查开发有限公司, 北京 100010,五矿勘查开发有限公司, 北京 100010
Geology, isotopic geochemistry and metallogenesis of Huaishuping gold deposit in Songxian County, Henan Province
WANG JiongHui,CHEN Liang,SU QiangWei,WANG HaoRan,LIU YunFei,LAI ShouHua
(China University of Geosciences, Beijing 100083, China;Minmetals Exploration and Development Co., Ltd., Beijing 100010, China;State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China)
本文二维码信息
码上扫一扫!

摘要
图/表
参考文献
相似文献

摘要点击次数: 1512   全文下载次数: 2070   点此下载全文
投稿时间:2015-05-15   修订日期:2016-02-14      网络发布日期:2016-06-30
中文摘要:河南嵩县槐树坪金矿床是豫西地区近年来通过勘查找矿评价出来的大型金矿床,该矿赋存于中元古界熊耳群火山岩地层,受断裂构造控制,与燕山期酸性岩浆侵入活动密切相关,是典型的构造蚀变岩型金矿床。矿区断裂构造可分为陡倾切层断裂和缓倾层间破碎带2种类型,缓倾层间破碎带是最重要的控矿和容矿构造,也是实现找矿突破的关键。氢、氧同位素分析显示,石英的δ18OV-SMOW值变化于10.1‰~14.4‰,成矿流体δ18OH2O变化于-1.3‰~7.3‰,δD变化于-95‰~-81‰;矿石硫同位素分析显示,δ34S值变化于-7.7‰~-1.4‰;矿石铅同位素分析显示,206Pb/204Pb变化于16.990~18.761,207Pb/204Pb变化于15.368~15.622,208Pb/204Pb变化于37.471~38.730。研究结果表明,槐树坪金矿床的成矿流体主要由岩浆水和大气降水组成,成矿主阶段以岩浆水为主,晚期有较多大气降水的加入;成矿物质主要来源于(直接或间接)太华群地层。该矿床的成矿过程经历了早期变形、变质作用的预富集,并于中生代后碰撞伸展构造环境下大规模富集成矿。
Abstract:The Huaishuping gold deposit in Songxian County of Henan Province is a large-size gold deposit found by exploration work in recent years. It is hosted by the Mesoproterozoic Xiong'er Group and closely related to the Mesozoic magmatism. The orebodies are controlled by faults. It is a typical tectonic altered rock type gold deposit. The fault in the mining area can be divided into steeply inclined incision faults and gently inclined interformational faults, with the latter being the most important ore-controlling and ore-bearing structure. And this is the key to achieving breakthrough in prospecting. Oxygen and hydrogen isotope data from quartz show that the δ18OV-SMOW values range from 10.1‰ to 14.4‰, δ18OH2O values from -1.3‰ to 7.3‰, and δD values between -95‰ and -81‰. The δ34S values of sulfides range from -7.7‰ to -1.4‰. Among Pb isotopes, the 206Pb/204Pb and 207Pb/204Pb ratios of sulfides are in the range of 16.990 to 18.761 and 15.368 to 15.622, respectively, and 208Pb/204Pb ratios from 37.471 to 38.730. The authors revealed that the ore-forming fluids of the Huaishuping gold deposit were composed of magmatic and meteoric water, the ore-forming fluid of main metallogenic stage mainly came from the magma, with the addition of more meteoric water at the late stage. The ore-forming materials were mainly derived from the Taihua Group. The Huaishuping gold deposit underwent preconcentration at the early stage by deformation and metamorphism, and large-scale gold enrichment and mineralization took place in a post-collisional extensional setting in Mesozoic.
文章编号:    
中图分类号:P618.51     
文献标志码:

基金项目:本文得到"河南嵩县金多金属矿集区成矿规律研究及找矿预测"项目资助
引用文本:
王炯辉,陈良,苏蔷薇,王浩然,刘云飞,来守华.2016.河南省嵩县槐树坪金矿床地质、同位素地球化学特征与成矿作用[J].矿床地质,35(3):524~538
WANG JiongHui,CHEN Liang,SU QiangWei,WANG HaoRan,LIU YunFei,LAI ShouHua.2016.Geology, isotopic geochemistry and metallogenesis of Huaishuping gold deposit in Songxian County, Henan Province[J].Mineral Deposits35(3):524~538
图/表
您是第241158869位访问者  京ICP备05032737号-5  京公网 安备110102004559
版权所有:《矿床地质》编辑部
主管单位:中国科学技术协会 主办单位:中国地质学会矿床地质专业委员会 中国地质科学院矿产资源研究所
地  址: 北京市百万庄大街26号 邮编:100037 电话:010-68327284;010-68999546 E-mail: minerald@vip.163.com
本系统由北京勤云科技发展有限公司设计 
手机扫一扫