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.
出处
《地质找矿论丛》
CAS
CSCD
2010年第2期112-117,共6页
Contributions to Geology and Mineral Resources Research
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
Lianbaling-Dongtuanbu area
gold-pollymetallic deposit
the metallogenic feature
the metallogenic model
the ore-searching direction
Hebei province
