摘要
和平铁矿赋存于三叠系下统布伦组一段底部,为一沉积型混合铁矿床。受晚石炭世古风化壳地形地貌的影响,矿体沿走向厚度变化很大,在古风化壳的低凹地带,矿体厚度较大,而在古化壳的突起地段,矿体厚度较薄。
Heping Fe deposit is in Lower Triassic Bulun Formation Member I＇ s bottom, which is a sedimen- tary mixed Fe deposit. Because of the influence of geomorphology of Late Carboniferous alaeo-weathering crust, the ore body changes very evidently along the strike. The ore body is thicker in the low part of palaeo-weathering crust, whereas it is thinner in the high part.
出处
《云南地质》
2015年第1期109-113,共5页
Yunnan Geology
关键词
层位控制
古风化壳
沉积型铁矿床
云南香格里拉和平
Horizon Control
Palaeo-Weathering Crust
Sedimentary Fe Deposit
Heping,Xianggelila, Yunnan
