摘要
穆家庄铜矿床位于东秦岭区的南秦岭造山带北缘，柞水多金属成矿带中部。区内构造发育，矿体产出基本受构造破碎带控制。认为属沉积-改造型矿床。从构造特征及演化角度浅析构造和成矿关系，认为加强构造研究将促进铜矿找矿的突破。
The Mujiazhuang copper deposit is located on the north margin of the southern Qinling orogen in the eastern Qinling area and at center of the Zashui polyimetallic ore belt. The ore bodies are coritrolled by structures which are well developed. It is an origin of structuretation- reformation. Based on analysis on structures and their relation to mineralization, it is held that the intensive research on structure favours breakthough of prospecting.
出处
《矿产勘查》
1999年第1期10-15,共6页
Mineral Exploration
关键词
穆家庄
铜矿床
同生断裂
秦岭
Mujiazhuang
copper deposit
contemporaneous fault
Qinling
