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首页> 外文期刊>Journal of Geology and Mining Research >Coarse-grained rutile from regolith in Ebensuk west of Tinto, Cameroon
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Coarse-grained rutile from regolith in Ebensuk west of Tinto, Cameroon

机译:从喀麦隆西部的eBensuk的eBensuk的粗粒粗糙的金红石

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Coarse rutile with some grains exceeding 32 mm was recovered from regolith excavated from three pits (ABC) at Ebensuk. The rutile concentration ranges from 2.53 kg/m3 of regolith material in Pit C to 2.83 kg/m3 in Pit B with an average of 2.66 kg/m3. The rutile is black, longitudinally striated, with a metallic to adamantine luster and hard. Results of grain size (Z) analysis show that the rutile crystals range in size from 4mm to Z32 mm. The grains are predominantly concentrated in the 16Z<32 mm size grade with a wt% of 48.3 followed by Z32 mm and 8Z 96 wt%, and subordinate Fe2O (2.2-3.1 wt%), and minor amounts of Al2O3, SO3, K2O P2O5 and Mn2O3 for all the samples analyzed, and meets international specifications for economic rutile ores. The rutile must have been derived through weathering of the underlying gneisses and their coarse nature is probably indicative of a possible source from granite pegmatite veins occurring in the gneisses outcropping in the study area.
机译:从eBensuk的三个凹坑(ABC)挖掘出来的凝雾度回收了超过32mm的粗红。金红石浓度范围为2.53kg / m 3的坑B中的氨基裂解材料,平均为2.66kg / m 3。金红石是黑色的,纵向横纹,具有金属到金刚石光泽和硬。晶粒尺寸(Z)分析结果表明,金红石晶体范围为4mm至Z32mm。晶粒主要集中在16z <32mm尺寸的级别中,WT%的48.3级,然后是Z32mm和8z 96wt%,并从属Fe 2 O(2.2-3.1wt%),少量Al 2 O 3,SO 3,K 2 O P2O5和分析所有样品的MN2O3,并满足经济金红石矿石的国际规范。金红石必须通过潜在的外形风化来源性,并且它们的粗糙性可能表明来自在研究区域的片状露头中出现的花岗岩柚子静脉的可能源。

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