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.
出处
《辽宁地质》
2000年第4期241-244,303,共5页
关键词
金银矿床
多金属矿床
成因
找矿方向
浊积岩
Qingchengzi
Au-Ag and polymetal
turbitide-type deposit
metallogenetic series
ore-prospecting direction
