式可布台铁矿地质特征及成矿模式  

The Geological Characteristics and Metallogenic Model of Shikebutai Iron Ore

作　　者：贺飞[1] 弓小平[1] 韩琼[1] 刘学良[1] 宋相龙[1] 

机构地区：[1]新疆大学,新疆乌鲁木齐830046

出　　处：《新疆地质》2013年第3期186-189,共4页Xinjiang Geology

基　　金：中国地质调查局项目"西天山阿吾拉勒成矿带铁矿成矿条件;成矿规律与勘查示范研究"(资[2010]矿评01-03-26)项目资助

摘　　要：式可布台铁矿床是西天山阿吾拉勒铁铜成矿带上发现较早、规模较大的赤铁矿矿床,是我国著名富铁矿床。该矿床矿石类型主要为赤铁矿,次为褐铁矿、镜铁矿及菱铁矿和磁铁矿。经矿床特征分析认为,成矿主要物质来源于上石炭统依什基里克组,构造活动为重要的控矿因素,结合成矿地质背景与控矿因素总结成矿模式,指出了找矿标志。Shikebutai Iron ore was the earlist and the largest scale hematite ore deposit found in west tianshan awulale iron copper metallogenic belt. It is a famous high-grad iron ore deposit in our country. The main ore type is hematite, sec- ondly are limonite, specularite, siderite and magnetite. The analysis of the deposit features that the mainly metallogenic main material comes from the upper Carboniferous Yishijilike assorted base rick formation,the structural movement is the important ore-controlling factors. Combined with the ore-forming geological background and ore-controlling factors can summarized the metallogenic model, and points out the prospecting marks.

关 键 词：式可布台铁矿 赤铁矿 地质特征 成矿模式 

分 类 号：P618.31[天文地球—矿床学]