辽宁营口地区中生代花岗岩类的成因及其含金性

    GENESIS AND GOLD CONTENT OF MESOZOIC GRANITOID IN YINGKOU DISTRICT LIAONING PROVINCE

    • 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。

       

      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.

       

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