新疆南天山东段红山金矿床地质特征  

THE GEOLOGICAL CHARACTERISTICS OF HONGSHAN GOLD DEPOSIT IN THE EASTERN PART OF SOUTH TIANSHAN, XINJIANG

作　　者：毕承彬 熊晓明 

机构地区：[1]江西地质矿产勘查开发局916大队

出　　处：《江西地质》1996年第2期101-110,共10页Jiangxi Geology

摘　　要：本文重点介绍了红山金矿床的地质特征，初步探讨了红山金矿矿床成因、金的富集规律及找矿标志。笔者认为红山金矿床金的成矿作用主要受韧性剪切带构造的控制，后期的脆性断裂及其所形成的构造岩是金的主要赋矿部位，金的成矿物质主要来自于闪长玢岩。The geological characteristics, deposit genesis, enrichment regularity of gold and prospecting criteria of Hongshan gold deposit have been discussed in this paper, The authors hold that the ore-forming process of gold in Hongshan gold deposit was mainly controlled by the ductile shear zone, the brittle fracture of the later stage and the tectonite formed by it are the major hosting parts. The orewforming materials of gold were derived from the dioritic porphyrite.

关 键 词：金矿床 地质特征 岩金 控矿条件 找矿方向 

分 类 号：P618.510.2[天文地球—矿床学] P618.510.8[天文地球—地质学]