CAJ | 학술논문

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。
호북성운서현서부지구제광상（점）산우상고생계니분계지층중，성광수지층화구조쌍중제약。로사엄-왕가장복식배사위광대공광구조，복식배사중적차일급배사위광상공광구조。배사중적단렬위광체공광구조。제、금（잡림형）광상（점）종서향동，유금-금제-제적분대규률。재철산조중종상도하，위금-금제-제적분대성。성광시대위연산기。
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 min-eralization age is Yanshanian .