本文已被：浏览 943次 下载 0次
中文摘要: S-C组构广泛存在于冀东地区，通过对谢杖子铜矿区、三家金矿区和兴隆北部三个地区的S-C组构分析和研究，发现矿体的厚度变化和展布形态严格受S-C构造控制，渗透性较差的岩石，如片麻岩、片岩中发育的S-C构造更容易成矿，一般在C构造面或C构造面与S构造面交汇的部位成矿条件最好。
Abstract:S-C fabric exists widely in East Hebei Province. Through the research and analysis to the S-C fabric in Xiezhangzi Copper Deposit, Sanjia Gold Deposit and North Xinglong area, it can be concluded that the thickness of ore body and distribution shape is strictly controlled by S-C structure. Low permeability rocks, such as the S-C structure developed in gneiss and schist, are more easily mineralized. Generally, the best metallogenic condition appears at C structural surface or the interface of C and S structural surface.
文章编号： 中图分类号： 文献标志码：
基金项目:国土资源部公益性行业科研专项项目( 201011013-3)和国家重点基础研究发展规划“973”项目( 2011CB403103)
| Author Name | Affiliation |
引用文本：
林 鑫,唐菊兴,张 志,宋俊龙,王红星.西藏尕尔穷铜金矿床IOCG矿体地质特征与成因[J].有色金属（矿山部分）,2014,66(4):38-46.
.Geological characteristics and origin of IOCG ore body in Gaerqiong Copper-Gold Deposit, Tibet[J].NONFERROUS METALS(Mining Section),2014,66(4):38-46.
林 鑫,唐菊兴,张 志,宋俊龙,王红星.西藏尕尔穷铜金矿床IOCG矿体地质特征与成因[J].有色金属（矿山部分）,2014,66(4):38-46.
.Geological characteristics and origin of IOCG ore body in Gaerqiong Copper-Gold Deposit, Tibet[J].NONFERROUS METALS(Mining Section),2014,66(4):38-46.
关注微信公众号