新疆阿尔泰造山带南缘金矿构造-流体-成矿作用  

THE SOUTH FRINGEOF XINJIANG ALTAI OROGENIC BELT GOLD MINE STRUCTURE-FLUID-MINERALIZATION

作　　者：木合塔尔．买买提 桑树勋[1] 木合塔尔．扎日 

机构地区：[1]中国矿业大学资源与地球科学学院,江苏徐州221116 [2]新疆大学地质与勘查工程学院,新疆乌鲁木齐830046

出　　处：《新疆地质》2009年第1期38-42,共5页Xinjiang Geology

基　　金：国家自然科学基金项目(40862006);新疆维吾尔自治区科技厅少数民族特培计划项目(200823119);自治区高校重点项目(XJEDU2006Ⅰ06)联合资助

摘　　要：新疆阿尔泰造山带南缘包括额尔齐斯构造带,为重要金矿床成矿带之一.文章以研究区成矿地质背景及成矿特征为基础,应用金矿成矿过程中构造-流体-成矿作用理论,对阿尔泰造山带南缘金矿成矿规律进行分析和探讨,提出了阿尔泰造山带南缘山-盆转换系统内金的构造-流体-成矿作用体系中构造主导作用、流体直接作用及构造和流体耦合作用与金矿成矿机理和时空分布特征间的关系.The Altai orogenic belt of Xinjiang is that has great difference compared with classical orogenic belt and it has unique geological features,its south edge include the Ertix tectonic belt that is one of the most important gold deposit metallogenic belt,so it has very great theory and actual（reality） research meaning. The article take studies the area mineralization geology background and the mineralization characteristic as a foundation, the use of gold mineralization in the process of structure - fluid - mineralization of the theoretical research methods, analyze and visit the theory of gold mine mineralize law for southern margin of the Altai orogenic belt, have put forward the leading role of the structure among the gold structure - fluid - mineralization system in the south edge of Altai orogenic belt mountain - basin converting system and fluid direct action ,as well as relations between structure and fluid coupling function with gold ore mineralization mechanism and space-time distribution characteristics.

关 键 词：阿尔泰造山带 金矿 成矿背景 构造-流体-成矿作用 

分 类 号：P618.51[天文地球—矿床学]