辽宁青城子矿田浊积岩型金银多金属矿床  

TURBIDITE-TYPE GOLD，SILVER AND POLYMETALLIC DEPOSITS IN QINGCHENGZI OREFIELD IN LIAONING

作　　者：陈江[1] 

机构地区：[1]东北大学资源与土木工程学院,辽宁沈阳110006

出　　处：《辽宁地质》2000年第4期241-244,303,共5页

摘　　要：辽宁东部赋存大面积的浊积岩，在浊积岩建造中产有铅锌矿床。近年来在青城子地区除发现铅锌矿床之外还发现了大型的金、银矿床。本文对典型的浊积岩型金、银多金属矿床进行了初步研究，概述了浊积岩型矿床的成因，认为辽宁东部原辽河群是浊积岩型矿床产出的有利场所，在浊积岩发育区进行找矿将能取得较大的突破。There exists a large scale of turbidite in East Liaoning,in which occur lead-zinc deposits.In recent years, a large scale Au-Ag deposit also has been found near the Qingchengzi lead-zinc deposits.The paper preliminarily studys the typical turbitide-type Au-Ag and Pb-Zn deposits,discusses the genesis of turbitide-type deposits.It is considered that turbidite-developing area of Liaohe Group in East Liaoning is favourale to further search for turbidite-type Au-Ag and polymetallic deposits.

关 键 词：金银矿床 多金属矿床 成因 找矿方向 浊积岩 

分 类 号：P618.5[天文地球—矿床学]