摘要
清镇猫场铝土矿是重要的铝土矿产地,红花寨、白浪坝矿段是猫场铝土矿的两个矿段,其含矿岩系为石炭系九架炉组(C1jj);矿体厚度随岩溶起伏面的变化而变化,矿体主要呈似层状、透镜状产出。铝土矿的形成受大地构造位置、古地貌、古地理、古气候等因素的控制,其成矿时代为早石炭世九架炉期。
Maochang bauxite deposit in Qingzhen City is an important production area of bauxite ores with Honghuazhai and Bailangba ore blocks being its two vital ore blocks. Its ore-beating rock series is C ljj and its ore-body thickness changes with the fluctuation of the karsts. The ore-body produced here are mainly in quasi-lamellar and tenticular formations. Having been controlled by the tectonics, ancient landform, paleogeography, and ancient climate as well as other factors, the ore-forming age of this bauxite ore deposit is in the Jiujialu period of early carboniferous age.
出处
《有色金属文摘》
2015年第3期75-76,共2页
Nonferrous Metals Abstract
关键词
铝土矿
成矿特征
控矿因素
bauxite deposit
metallogenic characteristics
ore-controlling factors
