【摘要】 湖北省郧西县西部地区锑矿床(点)产于上古生界泥盆系地层中,成矿受地层和构造双重制约。老寺厂—汪家场复式背斜为矿带控矿构造,复式背斜中的次一级背斜为矿床控矿构造。背斜中的断裂为矿体控矿构造。锑、金(卡林型)矿床(点)从西向东,有金—金锑—锑的分带规律。在铁山组中从上到下,为金—金锑—锑的分带性。成矿时代为燕山期。更多还原

【Abstract】 Gold-stibium deposit(point) is produced in the upper Paleozoic of Devonian strata at Yunxi of Hubei. The Laoshichang-Wangjiachang of complex anticline is ore-controlling structure of ore belt and the secondary anticline in the complex anticline is the ore controlling structure. The fault in the anticline is the ore controlling structure of deposit.There is Carlin type of gold deposit. Stibium and gold deposit(point) show the gold-gold-stibium-stibium zoning law from west to east. Deposit show the gold-gold-stibium-stibium zoning law in the Tieshan Formation from top to bottom. Its mineralization age is Yanshanian.更多还原