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庞家沟银多金属矿地质特征及成因浅析
引用本文:王荣全,葛之亮,贾继标. 庞家沟银多金属矿地质特征及成因浅析[J]. 矿产与地质, 2007, 21(3): 270-274
作者姓名:王荣全  葛之亮  贾继标
作者单位:天津华北地质勘查总院燕郊综合勘查院,河北,燕郊,065201
摘    要:庞家沟银多金属矿床受断裂构造和岩性双重控制,其矿种及其成因在冀北地区具有代表性.从阐述庞家沟银多金属矿地质特征入手,分析、研究其矿床成因.结果认为,该矿床为燕山晚期热液矿床.

关 键 词:银多金属矿床  矿床成因  地质特征  庞家沟
文章编号:1001-5663(2007)03-0270-05
收稿时间:2007-02-21
修稿时间:2007-02-21

Geological characteristics of Pangjiagou silver polymetallic deposit and its genesis
WANG Rong-quan,GE Zhi-liang,JIA Ji-biao. Geological characteristics of Pangjiagou silver polymetallic deposit and its genesis[J]. Mineral Resources and Geology, 2007, 21(3): 270-274
Authors:WANG Rong-quan  GE Zhi-liang  JIA Ji-biao
Affiliation:Yanjiao Comprehensive Exploration Institute of Tianjing North China General Geological Exploration Institute, Yanjiao, Hebei 065201,China
Abstract:Pangjiagou silver polymetallic deposit is jointly controlled by fracture and lithology. The ore species and genesis of ore are typical in North Hebei region. Its genesis was analyzed and studied according to the geological characteristics of the deposit. It was concluded that the deposit belongs to thermal deposit of Late Yanshanian period.
Keywords:silver polymetallic deposit   genesis of deposit   geological characteristics   Pangjiagou
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