학술논문
湖北省郧西县西部地区锑矿地质特征及成矿规律 / Geological Features and Metallogenic Regularities of Stibium Deposit at West of Yunxi of Hubei
Document Type
Academic Journal
Source
资源环境与工程 / Resources Environment & Engineering. (6):749-756
Subject
Language
Chinese
ISSN
1671-1211
Abstract
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。
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 .
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 .