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The gypsum mineralization in the Nigerian sector of Chad Basin was believed to have been a product of diagenesis but the laminar primary structures on all the gypsum forms, the location of the gypsum mineralization in shallow ares around a basement dome that separates two sedimentary basins, and the quantity of the mineralization compel us to think of another origin for primary gypsum mineralization. The presence of the laminations on each gypsum form besides the diagenetic features predates the mineralizat

Author
ATBU_Dr_Ahmed
Language
EN

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