辽宁抚顺县傲牛铁矿矿床地质特征分析  

Analysis of geological characteristics of iron ore deposit in Fushun County, Liaoning

作　　者：王爱博 

机构地区：[1]抚顺罕王傲牛矿业股份有限公司,辽宁抚顺113000

出　　处：《世界有色金属》2017年第10期272-273,共2页World Nonferrous Metals

摘　　要：矿区内含矿层位主要分布在中部地层,即于混合质角闪斜长片麻岩夹混合质变粒岩中。从区域地层对比来说,相当于鞍山群什村组地层中部层位,构成NWW-SEE磁铁石英岩带。除局部倒转外大致作220°-230°倾斜,产状较陡,倾角65°-85°,呈多层状磁铁石英岩扁豆体(群)产出。经工作由工业价值的32个矿体中,以Fe1、Fe2、Fe14、Fe15四个矿体具有一定规模,为矿区内主要主要矿体。The formation of seam position containing mining area is mainly distributed in the middle, in hybrid hornblende plagiogneiss with mixed granulites in. From the regional stratigraphic correlation, the equivalent of what village Anshan group strata in the middle layer, a NWW-SEE magnetite quartzite belt. In addition to the local inversion, the slope is roughly tilted at 220 degrees-230 degrees, and the occurrence is steeper. The dip angle is 65 degrees-85 degrees, showing the output of multi layered magnetite, quartz, hyacinth bean（group）. After the 32 ore bodies of industrial value, the four orebodies, Fe1, Fe2, Fe14 and Fe15, are of a certain size, and are the main ore bodies in the mining area.

关 键 词：鞍山群通什组地层 黑云角闪斜长片麻岩 似层状矿 变粒岩 

分 类 号：P618.31[天文地球—矿床学]