Petrography, mineralogy and geochemistry of Cretaceous sediment samples from western Khorat Plateau, Thailand, and considerations on their provenance
Review articleOpen access

Highlights•Geochemistry suggests the passive continental margin of the Khorat Plateau.•Geochemistry and mineralogy indicate granite, granodiorite or pegmatite sources.•High silica content and high maturity index indicate the sediment reworking.•CIA values represent high degree of weathering of the different source areas.

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