摘要
彩石沟铁矿位于阿尔金北缘沟口泉地区,为2008年新发现的小型铁矿床.该铁矿层产于硅质岩中的含铁硅质岩建造.铁矿层、含铁硅质岩、硅质岩呈中薄层状互层产出,局部地段铁矿层较富集.通过分析研究该矿床地质和物性特征,结合已有铁矿床进行对比研究,初步总结该矿床成因.认为彩石沟铁矿为阿尔金白尖山铁矿带西延.
The Caishigou iron deposit is located in Goukouquan area , the northern margin of Altyn mountain, as a small-sized one found in 2008,The iron deposit found in silicilith and form of silicalite formation. Thin layer rocks include interbedding of iron horizon and iron-bearing siliceous rock and silicilith, iron horizon is enrichment in some local section. In this paper, based on the analysis of characteristics which include geology and physics, and a comparative study of existing deposits, preliminary summary of deposit genesis. The evidence showed that the Baijianshan iron ore belt have considerable stretch in the west.
出处
《新疆地质》
CAS
CSCD
北大核心
2012年第1期36-39,共4页
Xinjiang Geology
关键词
阿尔金山东段
彩石沟铁矿
含铁硅质岩
Eastern part ofAltyn mountain
Caishigou iron deposit
Iron-bearing siliceous rock
