摘要
卡拉麦里山是东准噶尔地区一个重要金成矿带,区内金矿类型较多,以变质碎屑岩型金矿为主.该类型金矿区域上受南部的卡拉麦里深断裂和北部的清水—苏吉泉大断裂控制,志留系、泥盆系和石炭系浅变质碎屑岩为区内主要赋矿地层,并与区内广泛分布的超基性岩有一定成因关系.近二年发现的双泉变质碎屑岩型金矿规模有望达到大型,打开了东准噶尔地区的金矿找矿局面,启示该区寻找此类金矿有较大的前景.
Kalamely Mountain is an important gold metallogenic belt in the East Jungger of Xinjiang .There are many types of gold deposits in the area and the main type of gold deposit is metamorphic clasolite type. This type of gold deposit is confined to the main southern fault of Kalamely and the main northern fault of Qinshui-Sujiquan. The main host strata are Silurian, .Devonian and Carboniferous and it there is a broad genetic relationship with the ultrabasic rocks. The metamorphic clasolite gold deposit found in the last two years at Shuangquan by prospecting will be a large scale deposit. It is evidence that the area is prospective for this type of gold deposit.
出处
《新疆地质》
CAS
CSCD
2005年第3期220-224,共5页
Xinjiang Geology
关键词
卡拉麦里山
变质碎屑岩型金矿
地质特征
成矿条件
双泉
Kalamely Mountain
metamorphic clasolite type of gold deposit
geological feature
metallogenic condition
Shuangquan
