甘肃红尖兵山脉型钨矿床地球化学特征  

Geochemical Features of Vein Type Tungsten Deposit of Mount Hongjianbing in Gansu Province

作　　者：李强[1] 司雪峰[1] 

机构地区：[1]甘肃省有色金属地质勘查局张掖矿产勘查院,甘肃张掖734012

出　　处：《甘肃冶金》2013年第2期58-61,共4页Gansu Metallurgy

摘　　要：红尖兵山脉型钨矿区地质、地球化学特征表明1/5万水系沉积物地球化学勘查在甘肃北山浅覆盖区是行之有效的勘查手段。总结该矿床地球化学特征,对明水-红尖兵山钨钼锡铋成矿亚带及成矿远景区的找矿具有指导意义。According to the geology and geochemical features of Mount Hongjianbing, it can be seen that sediment geochemi- cal exploration of 1/50 000 drainage system is an effective means of exploration in shallow coverage areas of North Mountain, Gansu. This paper summarizes the geochemical features of ore deposits and provides guidance to prospecting of the metallo- genic subzones and prospecting areas of Mingshui-Hongjianbing for tungsten, molybdenum, tin and bismuth minerals.

关 键 词：脉型黑钨矿 地质特征 地球化学 甘肃北山 

分 类 号：P618.67[天文地球—矿床学]