Journal of Geological Society of India (Online archive from Vol 1 to Vol 78)

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The sedimentary structures in the bauxite deposits of the Jammu area are suggestive of a reworked bauxite precursor. Trace elements and REE concentrations show that the precursor bauxite originated from the weathering of basalt. It means that the bauxite forms a part of the earliest interval of the Himalayan foreland sedimentary sequences.

Keywords

Bauxite, Reworked Basalt, Geochemistry, Sedimentary Structures, Jammu Area, Jammu and Kashmir.
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