CAJ | 학술논문

文章对大湖塘矿集区燕山期岩浆岩从岩体的空间分布、岩石的地球化学特征等方面进行了分析研究，探讨了岩浆岩的成因及其与成矿的关系。结果表明，该矿集区燕山期岩浆岩是一个半隐伏―隐伏的多次侵入的岩株状杂岩体，均属强过铝质的 S 型花岗岩，为岩浆成因，深熔浅成，形成于同碰撞构造环境。各期次岩体 W、Sn、Mo、Bi、Cu、Zn 等成矿元素含量高，矿床、矿体及矿床金属分带均围绕岩体展布，是成矿的母岩。成岩与成矿是先行后续的关系，成矿主要发生在燕山早期。
문장대대호당광집구연산기암장암종암체적공간분포、암석적지구화학특정등방면진행료분석연구，탐토료암장암적성인급기여성광적관계。결과표명，해광집구연산기암장암시일개반은복―은복적다차침입적암주상잡암체，균속강과려질적 S 형화강암，위암장성인，심용천성，형성우동팽당구조배경。각기차암체 W、Sn、Mo、Bi、Cu、Zn 등성광원소함량고，광상、광체급광상금속분대균위요암체전포，시성광적모암。성암여성광시선행후속적관계，성광주요발생재연산조기。
The distribution and geochemical characteristics of Yanshanian magmatic rocks in Dahutang ore-concentrated area are analyzed in this paper and the genesis of magmatic rocks and its relationship with min-eralization are discussed.The results indicate that Yanshanian magmatic rocks in this ore-concentrated area are a hemi-concealed to concealed stock-like complex body with s of intrusive ages.The rocks also show strongly peraluminous affinity and are classified into S-type granite.The area is magmatogenic,anatectic and supergene,and it is formed in the syn-collisional structural setting.Metallogenetic elements such as W,Sn, Mo,Bi,Cu and Zn are relatively high in rock bodies of each period,and deposit,ore-body and metalzoning of the deposit are distributed around rock body which is the ore-forming mother rock.The diagenetic process happened before the mineralization process.The main mineralization process occurred in Early Yanshanian stage.