衡阳盆地北缘盐田桥铜矿床成矿构造地质地球化学特征
发布时间：2019-02-27 16:29
【摘要】：盐田桥铜矿床位于长寿-衡阳-观音阁断裂成矿带中部,属茶恩寺铜铅锌多金属成矿区内,是以铜矿为主,共(伴)生有铅锌矿等高-中温热液充填交代型矿床。以构造地球化学找矿为出发点,在研究区域构造地质背景、矿区构造地质特征及控矿因素的基础上,重点对F_1断裂构造岩主量元素、微量元素特征进行了分析,发现F_1中Cu、Pb、Zn、W等成矿元素有较大变化,说明元素的富集与断裂的活动有着极为密切的成因关系。富含成矿元素热液沿F_1断裂消弱带运移,并充填到构造裂隙中,与围岩发生交代作用而富集成矿。
[Abstract]:The Yantianqiao copper deposit is located in the middle of the Changshou-Hengyang-Guanyingge fault metallogenic belt, which belongs to the Chainsi copper-lead-zinc polymetallic ore deposit. It is mainly copper deposit, and there are high-middle temperature hydrothermal filling and replacement deposits of lead-zinc ore. Based on the study of regional tectonic geological background, structural geological characteristics and ore-controlling factors, this paper focuses on the analysis of the main elements and trace elements of the tectonic rocks in FU1 fault, based on the structural geochemical prospecting. It is found that the ore-forming elements such as Cu,Pb,Zn,W and other metallogenetic elements have great changes, indicating that the enrichment of elements has a very close genetic relationship with the activity of the faults. The hydrothermal fluid rich in ore-forming elements migrates along the weakening zone of the Fx1 fault and fills in the structural fissures, where metasomatism occurs with the surrounding rock to enrich the integrated ore.
【作者单位】： 湖南省核工业地质局三0六大队;
【基金】：湖南省核工业地质局重点科研项目“湖南省衡阳盆地西北缘铜多金属矿成矿条件及成矿预测”(KY2014-306-01)
【分类号】：P618.41
[Abstract]:The Yantianqiao copper deposit is located in the middle of the Changshou-Hengyang-Guanyingge fault metallogenic belt, which belongs to the Chainsi copper-lead-zinc polymetallic ore deposit. It is mainly copper deposit, and there are high-middle temperature hydrothermal filling and replacement deposits of lead-zinc ore. Based on the study of regional tectonic geological background, structural geological characteristics and ore-controlling factors, this paper focuses on the analysis of the main elements and trace elements of the tectonic rocks in FU1 fault, based on the structural geochemical prospecting. It is found that the ore-forming elements such as Cu,Pb,Zn,W and other metallogenetic elements have great changes, indicating that the enrichment of elements has a very close genetic relationship with the activity of the faults. The hydrothermal fluid rich in ore-forming elements migrates along the weakening zone of the Fx1 fault and fills in the structural fissures, where metasomatism occurs with the surrounding rock to enrich the integrated ore.
【作者单位】： 湖南省核工业地质局三0六大队;
【基金】：湖南省核工业地质局重点科研项目“湖南省衡阳盆地西北缘铜多金属矿成矿条件及成矿预测”(KY2014-306-01)
【分类号】：P618.41
【相似文献】
相关期刊论文 前10条
1 ;中国铜矿开发开始重大战略西移[J];探矿工程(岩土钻掘工程);2010年10期
2 吴良土,裴荣富;对铜矿勘查的意见[J];中国地质;1989年10期
3 魏民;赵鹏大;王学平;刘红光;赵精满;杨丽沛;;中国大型—超大型铜矿床品位—吨位模型[J];地质论评;2000年S1期
4 唐俊华;长江中下游地区层状铜矿床基本特征及成因[J];矿产与地质;2000年02期
5 本刊编辑部;《铜矿地质译文集》简介[J];西北地质;2002年02期
6 薛步高;史料考证与找矿(之三):铜矿[J];云南地质;2002年03期
7 刘扬;世界上第二例大规模自然铜矿在我国被发现[J];有色设备;2002年05期
8 沈存利,苏宏伟,王守光;内蒙古铜矿床区域成矿特征初步研究[J];西北地质;2004年03期
9 崔银亮,秦德先,陈耀光,毛云忠;中国云南金平龙脖河铜矿与越南生权铜矿初步对比研究[J];地质与勘探;2004年06期
10 崔银亮;秦德先;高俊;杨学善;陈耀光;;云南金平龙脖河铜矿床与新平大红山铁铜矿床对比研究[J];中国工程科学;2005年S1期
相关会议论文 前10条
1 孙海田;韩发;葛朝华;;我国铜矿床主要类型及找矿方向初探[A];中国地质科学院文集（25）[C];1992年
2 宋学信;;筏子坝铜矿床(体)快速定位预测的综合示范研究[A];中国地质科学院“九五”科技成果汇编[C];2001年
3 徐文p，
本文编号：2431431
本文链接：https://www.wllwen.com/kejilunwen/diqiudizhi/2431431.html
