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Bauxite provinces of the world

Journal

GEOLOGY OF ORE DEPOSITS
Volume 51, Issue 5, Pages 339-355

Publisher

PLEIADES PUBLISHING INC
DOI: 10.1134/S1075701509050018

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Phanerozoic bauxite provinces are contoured and characterized. The relations to large tectonic units-ancient and young platforms, island arcs and foldbelts, active continental margins, etc.-are chosen as the major criterion for the recognition of bauxite provinces; 19 provinces of different age and conditions of bauxite deposition are described. Single- and multistage as well as single- and multilevel provinces are distinguished depending on the type of tectonic and geomorphic structure. The most productive bauxite provinces are located in the present-day tropical zone within ancient Gondwanan platforms. Three-level provinces with Cretaceous bauxite at the highest and oldest (post-Gondwanan) surface and Cenozoic deposits at lower and younger planation surfaces are predominant. The most complex, two- and three-stage and multilevel provinces are related to ancient fold regions. The single-level provinces are localized in young island arcs and oceanic islands. The prevalent genetic types of bauxite deposits-lateritic, sedimentary, and karst-are shown in the map of bauxite provinces.

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