摘要
该金矿为破碎带蚀变岩型金矿,地处丰宁-隆化深断裂和尚义-平泉深断裂之间,主要成矿带位于闪长岩体,变闪长岩体破碎蚀变带内。通过对区内控矿构造的研究,浅析该区的成矿特征及富集规律。
The gold mine of fracture zone altered rock type gold deposit, located in Feng Ning-Long Hua deep fracture monk righteousness-hiraizumi between deep fracture, the main metallogenic belt is located in the diorite rock, diorite rock broken alteration belt. The metallogenic characteristics and enrichment regularity of the area are analyzed through the study on the structure of the inner control.
作者
鲁一奇
LU Yi-qi(514 Brigade of N ortHChina Geological Exploration Bureau,Chengde 067000,China)
出处
《世界有色金属》
2018年第7期111-112,共2页
World Nonferrous Metals