辽宁清原大林子地区地质特征与找矿标志  

The Geological Characteristics and Prospecting Indicators of Dalinzi Area in Liaoning Province

作　　者：鞠传奇 肖政龙 JU Chuan-qi, XIAO Zheng-long(101 Team of The Bureau of Liaoning Non-Ferrous Geology, Fushun 113015,Chin)

机构地区：[1]辽宁省有色地质局一0一队,辽宁抚顺113015

出　　处：《有色矿冶》2018年第4期4-6,15,共4页Non-Ferrous Mining and Metallurgy

摘　　要：辽宁清原地区是我国重要的金铜多金属成矿区,大林子地区成矿地质背景较好,金矿化体产出于太古代花岗绿岩地体中。通过主持该项目野外综合地质工作,对该区的地质矿化体特征及找矿标志等进行了分析探讨,认为金矿(化)体与水系沉积物异常和土壤异常吻合度较高,矿化信息丰富,找矿标志明显。Qingyuan area is a very important gold copper polymetallic metallogenic zone in Liaoning province. The metallogenic background of this area is better, the gold mineralized body of Dalinzi area is found in Archean granite greenstone terrane. By hosting the field geological works of the project, the characteristics of geological mineralization and prospecting indicators factors in this area are analysed . It is considered that the coincidence degree between gold mineralized body and stream sediment anomaly and soil anomalous is high.The mineralization informations are rich and the prospecting indicators are obvious.

关 键 词：大林子地区 花岗绿岩地体 成矿地质背景 找矿标志 

分 类 号：P624[天文地球—地质矿产勘探]