摘要
新疆哈密市卓越铅锌矿位于塔里木板块北缘(Ⅰ),阿奇克库都克-沙泉子深大断裂南侧,中天山地块(Ⅱ)星星峡隆起带(Ⅲ)内^([1])。容矿地层为青白口系天湖岩群,含矿岩性为石榴透辉矽卡岩。文章通过对矿床地质特征和成矿背景的总结,初步确定该矿床为矽卡岩改造富集的喷流沉积型铅锌矿。
The lead zinc ore deposit in Xinjiang, Hami is located in the northern margin of the Tarim plate （Ⅰ）, the south side of the Achike Cu Duke sand fault, and the Middle Tianshan block （Ⅱ） . The ore bearing strata are the Qingbaikouan Lake rock group, ore bearing rock diopside skarn garnet. Based on the summary of the geological characteristics and metallogenic background of the deposit, this paper preliminarily determined that the deposit is a sedimentary lead-zinc deposit, which is enriched and transformed by the skarn.
出处
《世界有色金属》
2017年第11期110-111,共2页
World Nonferrous Metals
关键词
铅锌矿
矿床地质特征
SIP测深
找矿标志
lead zinc deposit
geological characteristics of ore deposit
SIP sounding
prospecting mark
作者简介
何跃，男，生于1992年，汉族，四川宣汉人，本科，助理工程师，研究方向：地质找矿。
