4.7 Article

Bauxitisation of anorthosites from Central Brazil

Journal

GEODERMA
Volume 167-68, Issue -, Pages 319-327

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.geoderma.2011.09.006

Keywords

Bauxite; Alitisation; Isalteritic transformation; Anorthosite; Barro Alto Complex

Categories

Funding

  1. CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)
  2. CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior)
  3. EDEM (Empresa de Desenvolvimento em Mineracao e Participacoes Ltda)

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Petrological studies using X-ray diffraction (XRD), X-ray fluorescence (XRF), optical microscopy, scanning electron microscopy (SEM-EDS) and electron microprobe analyzer (WDS) showed the mineralogical, micromorphological and geochemical transformations due to the bauxitisation of anorthosite from the Barro Alto Stratiform Mafic-Ultramafic Complex (Central Brazil). The hydrolytic alteration of the anorthosite occurred in two different stages in accordance with the order of stability of the minerals to the weathering: firstly the bytownite and secondly the ferromagnesian minerals. The weathering solutions, benefited from the existing network of fractures, percolated the weakness zones of the minerals characterising the microsystem of contact in which cores of plagioclase and ferromagnesian minerals were formed. In the first stage, the plagioclases are altered directly to gibbsite, and at an early stage, during the change process, the gibbsite crystals surround the primary ferromagnesian minerals that are totally or partially preserved. The transformation is isalteritic and is responsible for formation of porous alteromorphs consisting of septa of coarse gibbsite and fine gibbsite. As the weathering process advances, the ferromagnesian minerals directly enter to goethite. The boxworks of gibbsite and goethite characterise a primary plasmic microsystem. (C) 2011 Elsevier B.V. All rights reserved.

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