玲珑矿田东风矿区深部及外围成矿规律研究  

Study on deep and peripheral metallogenic regularity of Dongfeng Mining area in linglong ore field

作　　者：王汝杰 杨松林 程东江 曹瑞 WANG Ru-jie;YANG Song-lin;CHENG Dong-jiang;CAO Rui(Qingdao Institute of Geological Engineering investigation,Qingdao,Shandong 266000,China;Yantai Gold Vocational College,Yantai,264000,China)

机构地区：[1]青岛地质工程勘察院,山东青岛266000 [2]烟台黄金职业学院,山东烟台264000

出　　处：《世界有色金属》2019年第18期238-238,242,共2页World Nonferrous Metals

摘　　要：通过对东风金矿床的地质特征、控矿因素及矿床成因的系统研究,提出应该进一步查证地球物理化学异常;同时本次研究分析东风矿区矿体特点,认为矿区NNE向断裂与其他方向断裂交汇部位为金矿的有利赋矿部位,是适宜于成矿物质富集的引张扩容空间。Based on the systematic study of geological characteristics,ore-controlling factors and genesis of Dongfeng gold deposit,it is proposed that geophysical and chemical anomalies should be further verified.At the same time,the characteristics of Dongfeng gold deposit are analyzed in this study.It is concluded that the intersection of NNE-trending faults and other faults in the mining area is a favorable ore-hosting site for gold deposits,which is suitable for formation.The expansion space of mineral enrichment.

关 键 词：地层 破头青断裂 玲珑花岗岩 尖灭再现 

分 类 号：P618.51[天文地球—矿床学]