新疆苏勒铁列克锡矿地质特征及找矿意义  

Geological characteristics and exploration significant of the Suletielieke tin deposit in Xinjiang

作　　者：万阈[1] 尤悦程 张魁召 王金生 刘闯 刘光红 尚丽 WAN Yu;YOU Yue-cheng;ZHANG Kui-zhao;WANG Jin-sheng;LIU Chuang;LIU Guang-hong;SHANG Li(No.7 Geological party,BGMERD of xinjiang,Wusu,83300)

机构地区：[1]新疆地质矿产勘查开发局第七地质大队,乌苏833000

出　　处：《矿产勘查》2018年第6期1152-1157,共6页Mineral Exploration

基　　金：新疆维吾尔自治区中央返还两权价款资金项目(编号:T15-2-LQ33)资助

摘　　要：新疆西天山苏勒铁列克锡矿是博罗科努Au-Cu-Mo-Pb-Zn-磷矿带西段新发现的锡矿床。文章基于详细野外地质调查,对矿床地质特征进行了总结,认为矿床赋存于晚石炭世花岗岩体与青白口系开尔塔斯群碳酸盐岩地层的接触带中,含矿地质体为锡石矿化石榴石透辉石矽卡岩,矿床成因属矽卡岩型锡矿。通过对矿床区域成矿环境的分析,认为应注意在科石琴山一带寻找与华力西中晚期S型花岗岩有关的矽卡岩型锡矿。The Suletielieke tin deposit,located in the western Tianshan of Xinjiang,represents the newly discovered tin deposit in the western part of the Boluokelu Au-Cu-Mo-Pb-Zn-P Metallogenic Belt. The author summarized the geological characteristics in accordance with detailed field survey and concluded that the ore body is hosted in the contact of the Qingbaikouan carbonate rocks of the Kelvin group and the late Carboniferous granitic intrusion. The mineralization mainly was contained in garnet-diopside skarns.Through the analysis of regional metallogeny,it is suggested that there is a great potential of exploration for skarn tin deposits that genetically related to middle to late Variscan S-type granites in the Keguqin Mountain region.

关 键 词：锡矿 地质特征 找矿意义 苏勒铁勒克 新疆 

分 类 号：P618.44[天文地球—矿床学]