关于新疆古伦沟铁铜矿成矿地质特征及找矿方向的探讨

Discussion on the geological characteristics and prospecting direction of the ancient Xinjiang iron ore deposit

巩乃斯石炭纪裂谷带以及依连哈比尔尕晚古生代沟弧带金、铅、锌、铜、钼成矿带是该矿大地构造所在,在其南部区域与阿吾拉勒-伊什基里克晚古生代弧后盆地金、铜、铁成矿带相邻(图1)。古伦沟铁铜多金属矿体,在花岗闪长岩以及灰白色薄层状微晶灰岩裂隙内以透镜状或者似层状特征进行分布,成因类型为后期热液型矿床。

Mine tectonic position for Yilianhabierga late Paleozoic trench arc belt, gold, lead, zinc, copper, molybdenum metallogenic belt and Runes Carboniferous Awulale rift zone, South - Yishijilike late Paleozoic arc basin of gold, copper and iron ore belt. The iron and copper polymetallic ore bodies in the paleo channel are layered and lenticular in the fracture of the white and thin bedded limestone and granodiorite.