青海省都兰县洪水河铁矿床成因及找矿远景探讨  

Investigation on the Hongshuihe iron deposit forming reason and ore-searching prospect in Dulan county of Qinghai Province

作　　者：保守礼 叶积龙[2] 祁俊霞 王春艳 吴远安 

机构地区：[1]青海省有色地质矿产勘查院,青海西宁810007 [2]青海省地质调查院,青海西宁810012

出　　处：《青海大学学报（自然科学版）》2010年第2期42-46,共5页Journal of Qinghai University(Natural Science)

摘　　要：通过分析洪水河铁矿地质特征、成矿地质背景和矿床地质特征,认为该矿床是沉积变质型铁矿床,进一步论述都兰县洪水河矿铁矿体在空间上为一个铁矿层,层位稳定,其延伸长,具有较大的找矿潜力。After the analysis on the Hongshuihe iron deposit geological feature,ore-forming geological background and the deposit geological characteristics,it is believed that this deposit is a sediment metamorphose type deposit.The iron ore body of Hongshuihe deposit is an iron deposit layer in space and the layer position is stable,the layer has a long extension and there is a good ore-searching potential.

关 键 词：洪水河铁矿床 沉积变质型 找矿潜力 

分 类 号：P61[天文地球—矿床学]