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Exploration and Sources of Bauxite Deposit in the Boloven Plateau, Southern Laos
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  • 英文篇名:Exploration and Sources of Bauxite Deposit in the Boloven Plateau, Southern Laos
  • 作者:Yongzhen ; Long ; Xiaoyong ; Yang ; Mu ; Yang ; Dexian ; Zhang
  • 英文作者:Yongzhen Long;Xiaoyong Yang;Mu Yang;Dexian Zhang;Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education,Central South University;School of Geosciences and Info-Physics, Central South University;CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences,University of Science and Technology of China;
  • 英文关键词:late ritic-type bauxite;;XRD;;datum processing;;exploration;;sources;;Boloven Plateau;;Laos
  • 中文刊名:Journal of Earth Science
  • 英文刊名:地球科学学刊(英文版)
  • 机构:Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education,Central South University;School of Geosciences and Info-Physics, Central South University;CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences,University of Science and Technology of China;
  • 出版日期:2019-02-01
  • 出版单位:Journal of Earth Science
  • 年:2019
  • 期:01
  • 基金:supported by Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University (No. 2018YSJS01);; the National Natural Science Foundation of China (No. 41673040);; the DREAM project of MOST China (No. 2016YFC0600404);; QingzhenYunfeng Aluminum and Iron Mining Co. (No. 738010033)
  • 语种:英文;
  • 页:129-138
  • 页数:10
  • CN:42-1788/P
  • ISSN:1674-487X
  • 分类号:P618.45
摘要
The Boloven bauxite deposit occurs either in the weathered basalt(alkali basalt and tholeiite), or in the Cretaceous sandstone. It is generally agreed that the bauxite deposits/laterites overlying the alkali basalt and tholeiite were derived from weathering of underlying basalt, however, the origin of bauxite deposit overlying the sandstone remains controversial. Chondrite-normalized REE patterns show that the bauxite ores/laterites overlying the sandstone exhibit quite similar chondrite-normalized REE patterns to those overlying the alkali basalt. Diagram of Al-Ti-Zr shows that the bauxite ores/laterites overlying the sandstone, tholeiite and alkali basalt are close to each other and to the calc-alkaline suite, however, significantly different from the sandstone and shales. Binary diagram of log Nb/Y vs log Zr/Ti further indicates that the parent rocks of bauxite ores/laterites overlying the sandstone belong to the suit of ultra-alkali to alkali basalt. Multivariate statistical analysis of geochemical data exhibit that the geochemical characteristics of HREE, Y, LREE and Al_2O_3 for bauxite ores/laterites overlying the sandstone are similar to those overlying the alkali basalt(15.7 Ma), obviously different from those overlying the tholeiite(1.2 to 0.5 Ma). Consequently, it can be inferred that the bauxite deposits/laterites overlying the sandstone were derived from the alkali basalt.
        The Boloven bauxite deposit occurs either in the weathered basalt(alkali basalt and tholeiite), or in the Cretaceous sandstone. It is generally agreed that the bauxite deposits/laterites overlying the alkali basalt and tholeiite were derived from weathering of underlying basalt, however, the origin of bauxite deposit overlying the sandstone remains controversial. Chondrite-normalized REE patterns show that the bauxite ores/laterites overlying the sandstone exhibit quite similar chondrite-normalized REE patterns to those overlying the alkali basalt. Diagram of Al-Ti-Zr shows that the bauxite ores/laterites overlying the sandstone, tholeiite and alkali basalt are close to each other and to the calc-alkaline suite, however, significantly different from the sandstone and shales. Binary diagram of log Nb/Y vs log Zr/Ti further indicates that the parent rocks of bauxite ores/laterites overlying the sandstone belong to the suit of ultra-alkali to alkali basalt. Multivariate statistical analysis of geochemical data exhibit that the geochemical characteristics of HREE, Y, LREE and Al_2O_3 for bauxite ores/laterites overlying the sandstone are similar to those overlying the alkali basalt(15.7 Ma), obviously different from those overlying the tholeiite(1.2 to 0.5 Ma). Consequently, it can be inferred that the bauxite deposits/laterites overlying the sandstone were derived from the alkali basalt.
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