花坤铜多金属矿区成矿规律及找矿方向  

Metallogenic regularity and prospecting direction of the copper polymetallic ore area of the Hua Kun

作　　者：张磊 ZHANG Lei(109 team of Liaoning Nonferrous Geological Bureau,Chaoyang 122000,China)

机构地区：[1]辽宁省有色地质局109队,辽宁朝阳122000

出　　处：《世界有色金属》2018年第1期88-89,共2页World Nonferrous Metals

摘　　要：通过对矿床的地质特征及诸多因素综合研究,认为花坤铜多金属矿属于构造—矽卡岩型矿床。归纳成矿与花坤杂岩体、围岩及旋卷构造的关系,总结成矿规律,探讨找矿方向。Through comprehensive study on the geological characteristics and many factors of the deposit,it is believed that the Hua Kun copper polymetallic ore belongs to the tectonic-skarn type deposit.The relationship between the mineralization and the Hua Kun complex,the surrounding rock and the spiral structure is summarized,and the metallogenic regularity is summarized and the prospecting direction is discussed.

关 键 词：花坤杂岩体 旋卷构造 围岩蚀变 

分 类 号：P618[天文地球—矿床学]