摘要
六叫沟金多金属矿位于华北陆块北缘。经地质调查及矿产勘查发现金铅锌矿体主要赋存于北东西向断裂构造带,铜矿体赋存于北东西向断裂构造带。目前矿体沿走向及倾向上均未得到工程控制。在分析六叫沟银铅锌矿成矿地质背景、矿体地质特征及物化探异常特征的基础上,提出了该矿与燕山期酸性火山-侵入活动有关,属中低温热液脉状充填型金多金属矿床,显示该区有较好的找矿前景。
six called ditch gold polymetallic ore is located in the North margin of North China land block.After Geological investigation and mineral exploration,it was found that gold,lead and zinc ore bodies were mainly found in the North East-West fault zone,and copper ore bodies were found in the North East-West fault zone.At present,the ore body has not been controlled by engineering along the direction and inclination.Based on the analysis of the geological background,geological characteristics and Geophysical anomalies of the Liumaigou silver lead-zinc ore deposit,it is proposed that the mine is related to the acidic volcano-intrusion activity in Yanshan period and belongs to the gold polymetallic deposit with low temperature hot liquid vein filling type.It shows that there is a good prospect of prospecting in this area.
作者
郜朋飞
权知心
王虎强
Gao Peng-fei;Quan Zhi-xin;Wang Hu-qiang(No.2 Geological Exploration institute of Henan Bureau of Geology and Minaral Resources,zheng zhou 460000 henan China;Shanxi Taiyuan Iron and Steel Group Co.,taiyuan 030000 shanxi China)
出处
《西部资源》
2020年第6期35-39,共5页
Western Resources
基金
乌兰察布市地质勘查项目管理中心基金项目(盟市政府委托)(编号:14-1-KC-3)。
关键词
六叫沟
金多金属矿
地质特征
找矿标志
内蒙古
Six called ditch
Gold polymetallic ore
Geological characteristics
Mining marks
inner mongolia
