CAJ | 학술논문

通过对乌兰乌珠尔-祁漫塔格地区华力西-印支期岩浆作用与成矿关系的分析和对比．进一步说明祁漫塔格东段早、中泥盆世侵入岩成矿作用不明显；早二叠世侵入岩形成的矿产不多，成矿作用一般；晚三叠世侵入岩在一定的围岩条件下常形成矽卡岩化，成矿作用较为明显．为该区主要成矿期；早侏罗世侵入岩的外接触带常形成矽卡岩化，成矿作用较好，也是测区内主要的成矿期之一。矿床类型以矽卡岩型为主。
통과대오란오주이-기만탑격지구화력서-인지기암장작용여성광관계적분석화대비．진일보설명기만탑격동단조、중니분세침입암성광작용불명현；조이첩세침입암형성적광산불다，성광작용일반；만삼첩세침입암재일정적위암조건하상형성석잡암화，성광작용교위명현．위해구주요성광기；조주라세침입암적외접촉대상형성석잡암화，성광작용교호，야시측구내주요적성광기지일。광상류형이석잡암형위주。
Analyzing the relationship between the magmatism and metallogenesis of Varisean-Indosinian stage in Wulanwuzhuer -Qimantage area shows that the metallogenesis of the intrusive rocks of early-medium Devonian epoch in eastern segment of Qimantage is not distinct;the metallogenesis of the intrusive rocks of early Permian epoch is normal;the intrusive rocks of late Trissie epoch is usually companied with skarnization under a certain wall rock condion. The metallogenesis is obvious and it is the main metallogenie epoch ; the cxsocontact zone of the intrusive rocks of early Jurassic epoch is usually companied with skarnization. The metallogenesis is better and it is also the main metallogenic epoch. The skarn type is the main deposit type.