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辽宁营口地区中生代花岗岩类的成因及其含金性
引用本文:刘斌,余昌涛.辽宁营口地区中生代花岗岩类的成因及其含金性[J].地质与资源,1993,2(2):118-126.
作者姓名:刘斌  余昌涛
作者单位:沈阳地质矿产研究所
摘    要:营口地区印支期花岗岩为Ⅰ型(同熔型)花岗岩,燕山期花岗岩为S型(陆壳改造型)花岗岩。印支期花岗岩是造山运动晚期岩浆作用的产物,岩浆来源于深部。燕山期花岗岩是与燕山期造山运动同构造期岩浆作用的产物,岩浆来源于浅部。金矿床的形成主要与印支期次碱性二长花岗岩岩浆作用有关。

关 键 词:中生代  花岗岩成因  含金性  辽宁营口  
收稿时间:1992-01-21

GENESIS AND GOLD CONTENT OF MESOZOIC GRANITOID IN YINGKOU DISTRICT LIAONING PROVINCE
Liu Bin Yu Changtao.GENESIS AND GOLD CONTENT OF MESOZOIC GRANITOID IN YINGKOU DISTRICT LIAONING PROVINCE[J].Geology and Resources,1993,2(2):118-126.
Authors:Liu Bin Yu Changtao
Institution:Shenyang institute of geology and mineral resources
Abstract:By studying the geology, petrology, petrochemistry and geochemistry of Mesozoic granitoids in Yingkou district, the authors believe the similarities.between Indosuiian granitoids in the studied district and I -type granite defined by Chappell and White,and between the Yanshanian granitoids and S -type granite in petrology .petrochemistry and geochemistry. The forming environment of ihe granitoids and its relationship with gold mineralization are discussed on the basis of the study of petrochemistry,Pb -isotope and gold content. The gold mineralization in this area is believed to be related to Indosinian granitic magmatism.
Keywords:Mesozoic genesis of granitoid Gold content Yingkou of Liaon-ng  
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