新全球动力学理论与成矿作用  

The New Global Dynamics Theory and Mineralization

作　　者：胡建卫 王宏君 杨志华[2] 李勇[2] 苏生瑞[2] 周义[2] 

机构地区：[1]新疆地质矿产勘察开发局,新疆乌鲁木齐830000 [2]长安大学,陕西西安710054

出　　处：《矿物岩石地球化学通报》2001年第4期337-343,共7页Bulletin of Mineralogy, Petrology and Geochemistry

基　　金：原地质矿产部秦巴 ( 85 0 1 0 18);国家自然科学基金 ( 4 92 72 136 );国家计委 ( 96 30 43);国家科委 ( 96 914 0 10 4);国土资源部 ( 95 0 2 0 0 2 0 1)资助项目

摘　　要：成矿作用的本质是成矿流体子系统在统一地质 成矿场中与其它子系统在远离平衡系统的动态过程中所能达到平衡的程度。成矿物质的来源和矿床的富集部位都受新全球动力学理论 -涡旋甩出说以及由它所决定的抽拉构造和多重岩片的控制。Mineralization itself means the content of equilibrium between the mineralizing fluid system in the universal geological-mineralizing field and its subsystem during the dynamic process far from equilibrium system. The sources of mineralizing materials and the enrichment position of ore-deposits could be well explained by the new global dynamic theory, that is, the theory of twisting vortex and throw-out as well as the drawing-out tectonics and multiple rock sheets determined by it.

关 键 词：动力学理论 统一地质-成矿场 成矿作用 多重岩片控矿论 抽拉构造 

分 类 号：P611[天文地球—矿床学]