陈庆刚,陈群,谢江涛.柬埔寨王国蒙多基里省红土型铝土矿矿床地质特征及成因浅析[J].贵州地质,2016,33(1):19-23
柬埔寨王国蒙多基里省红土型铝土矿矿床地质特征及成因浅析
Analyses of Deposit Characteristics and Genesis of Lateritic Bauxite in Mondulkiri Province,Cambodia
  
DOI:
中文关键词:  风化壳  红土型  三水铝石铝土矿床  蒙多基里  柬埔寨王国
英文关键词:Crust of weathering  Lateritic  Gibbsite  Bauxite deposit  Mondulkiri  Cambodia
基金项目:
作者单位
陈庆刚 贵州省地矿局115地质大队贵州清镇551400 
陈群 贵州省地矿局115地质大队贵州清镇551400 
谢江涛 贵州省地矿局115地质大队贵州清镇551400 
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中文摘要:
      柬埔寨王国红土型铝土矿,产于北东部蒙多基里高原,属第四系风化壳红土型三水铝石矿床,系玄武岩经风化作用残留而成。矿体呈面状分布于坡体顶部平缓台地区,厚度稳定,矿体分布受坡体展布形态制约,平面上受浅地表水系侵蚀呈不规则面状覆于地表、浅地表;矿床规模为大型,铝土矿资源量达数亿吨。
英文摘要:
      In Cambodia,the laterutic bauxite occurs in Mondulkiri highland,it is crust lateritic gibbsite of Quaternary system and formed by basalt weathering. The orebody distributes in the platform of slope as planar,the thickness is stable,the orebody distribution is restricted by the slope,the planar is irregular on the surface or shallow surface by the erosion of surface water. The scale is big and the resource is hundreds of million ton.
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