4.5 Article

Outline of Metallogenic Regularity of Bauxite Deposits in China

Journal

ACTA GEOLOGICA SINICA-ENGLISH EDITION
Volume 89, Issue 6, Pages 2072-2084

Publisher

WILEY-BLACKWELL
DOI: 10.1111/1755-6724.12618

Keywords

bauxite; deposit type; bauxite metallogenic belt; metallogenic series; metallogenic regularity

Funding

  1. Geological Survey Projects of the CGS [12120115065601, 1212011121037, 12120114039601, 121201120369]

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Among the abundant aluminum ore resources in China, bauxite is dominated, which is mainly distributed in 19 provinces and regions, including Shanxi, Henan, Guizhou and Guangxi. The major deposit type of bauxite is paleo-weathering crust sedimentary type, and the other one is the accumulation type. The main metallogenic period is the late Paleozoic Era followed by the Cenozoic Era. The metallogenic tectonic background is characterized by a cratonic environment. This paper summarizes the bauxite metallogenic regularity based on the characteristics of bauxite resources, bauxite deposit type, bauxite metallogenic belt and metallogenic series in China, and 15 bauxite metallogenic belts, 8 bauxite metallogenic series and 7 bauxite ore concentrated areas were identified in the study. This paper also provides a theoretical basis for the evaluation of the potential of bauxite resources.

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