新疆北部布尔克斯岱金矿地质地球化学特征及其成矿作用  

GEOLOGICAL-GEOCH EMICAL CHARACTERISTICS AND MINERALIZATION OF THE BUERKSIDAI GOLD DEPOSIT IN NORTHERN XINJIANG

作　　者：谭克仁[1] 谢建华 吴堑虹[1] 潘传楚[1] 贺伯初 郭定良[1] 

机构地区：[1]中国科学院长沙大地构造研究所,长沙410013

出　　处：《大地构造与成矿学》1992年第3期239-251,共13页Geotectonica et Metallogenia

摘　　要：布尔克斯岱金矿床产于斋桑地洼区扎尔玛-萨吾尔地穹系.本文研究了该矿床区域大地构造、区域地质地球化学特征和矿床地球化学以及成矿作用,指出本矿床是地槽阶段断裂构造、沉积作用和地幔岩浆作用的综合作用的结果.The Buerksidai gold deposit is located in the Zhaerma—Sawuer geodome system, Zaisan diwa region. In this artical, the regional geotectonics, regional geotectonicgeochemical characteristics, geochemistry and mineralization of the deposit have been studied. It indicated that the gold deposit has resulted from the synthetic process of faulting, sedimentation and mantle magmatism in a geosynclinal stage.

关 键 词：金矿床 地质 地球化学 成矿作用 

分 类 号：P618.510.4[天文地球—矿床学]