河北省涞源县连巴岭—东团堡地区金-多金属矿地质特征及找矿方向  

THE GEOLOGICAL FEATURE AND PROSPECTING DIRECTION OF THE GOLD POLLYMETALLIC DEPOSITS IN THE LIAN BALING-DONGTUANBU AREA OF LAIYUAN COUNTY,HEBEI PROVINCE

作　　者：郭长华[1] 刘志明[1] 陆树文[1] 高州 郭培培[1] 

机构地区：[1]天津华北地质勘查总院,天津300181

出　　处：《地质找矿论丛》2010年第2期112-117,共6页Contributions to Geology and Mineral Resources Research

摘　　要：河北省涞源县连巴岭—东团堡地区金-多金属矿受王安镇岩体和雾迷山组白云岩的接触带、NE向乌龙沟深断裂的控制。区内发现4条NW向金-多金属含矿带,矿化产于构造蚀变带中或中酸性脉岩旁侧,与成矿有关的围岩蚀变为硅化、黄铁矿化和铁锰碳酸盐化等。建立了金-多金属矿的成矿模式,指出进一步找矿的方向。The gold pollymetallic deposits in the Lian Baling-Dongtuanbu area of Laiyuan county,Hebei are controlled by contact zone of Wanganzhen intrusive body and dolomite of Wumishan formation.4 gold pollymetallic ore-bearing belts trending in NW direction are discovered in the area with mineralization occurring in cataclastic alteration zones or near the intermediate-acidic dykes.The ore-related alterations are silicification,pyritization,Fe and Mn carbonation.Based on this the metallogenic model is set up and the ore-searching direction put forword.

关 键 词：连巴岭—东团堡地区 金-多金属矿 成矿地质特征 成矿模式 找矿方向 河北省 

分 类 号：P613[天文地球—矿床学] P618.51[天文地球—地质学]