辽宁东青堡银锌矿床地质特征及成因探讨

J4 ›› 2010, Vol. 18 ›› Issue (2): 45-50.

辽宁东青堡银锌矿床地质特征及成因探讨

警黄金第四支队，辽宁辽阳 111000

出版日期:2010-04-30 发布日期:2013-11-19

Geological Features and Genesis of Dongqingpu Silver-Zinc Deposit in Huludao City，Liaoning Province

NO.4 Gold Geological Party of CAPF，Liaoyang 111000，Liaoning，China

Online:2010-04-30 Published:2013-11-19

摘要/Abstract

摘要：

辽宁省葫芦岛市东青堡银锌矿床产于山神庙—钢屯—高桥EW向成矿带东段，是一处以银为主、伴生锌、铅、金的多金属矿床。全区共有3条工业矿体，产于雾迷山组燧石条带白云岩中，受近EW向基底断裂及其上盘的爆破角砾岩筒和花岗斑岩控制，成矿物质主要来源于地幔或下地壳，成矿热液来源于岩浆水。矿床成因类型为与酸性次火山岩和爆破角砾岩有关的中低温热液矿床。

关键词: 地质特征, 矿床成因, 中低温热液矿床, 东青堡银锌矿床, 辽宁省

Abstract:

Dongqingpu silver-zinc deposit occurs in the east section of Shanshenmiao-Gangtun-Gaoqiao metallogenic belt in Huludao City，Liaoning Province.It is a polymetallic deposit mainly with silver,associated zinc, lead and gold.There are three industry orebodies in this area, produced in bands dolomite in Wumishan Group, controlled by EW-trending basement fault（F1）and esplosive breccia pipe,granite porphyry in its hanging wall.The metallogenic material is mainly from mantle or lower crust,and the metallogenic hydrothermal is from magmatic water.So,we can see that the ore-forming type is a medium-low temperature hydrothermal deposit which is related to acidity sub-volcanic rock and esplosive breccia.

Key words: Geological features, Genesis, Medium-low temperature hydrothermal deposit, Dongqingpu silver-zinc deposit, Liaoning Province

李永维, 刘兴国, 郭长义. 辽宁东青堡银锌矿床地质特征及成因探讨[J]. J4, 2010, 18(2): 45-50.

LI Yong-Wei, LIU Xin-Guo, GUO Chang-Xi. Geological Features and Genesis of Dongqingpu Silver-Zinc Deposit in Huludao City，Liaoning Province[J]. J4, 2010, 18(2): 45-50.

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