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Iraqi National Journal of Earth Science

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Authigenic Minerals and Diagenesis in The Clastic Sediments of The Ghar Formation South and Southeast Iraq.

    Ali Al-Juboury Jamal S. Al-Ghrear Mohammad A. Al-Rubaii

Iraqi National Journal of Earth Science, 2003, Volume 3, Issue 1, Pages 1-21
10.33899/earth.2003.36680

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Abstract

Study of clay minerals (Kaolinite,Iillite and Illite-Smectite mixed layers) in the clastic sediments of the Ghar Formation (Upper Oligocene-Lower Miocene) is the main indicator for the variation of the pore waters responsible for the eodiagenetic processes affecting on
these sediments. Variation of these clay minerals are used also to distinguish the sedimentary environments of the Ghar Formation as transitional environment from fluvial into marine. The genetic relations of these clay minerals and their semi quantitative proportions by XRD and SEM are used also to distinguish the authigenic minerals and their paragenetic sequence.
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Keywords:
    Authigenic Minerals Formation Southeast Iraq
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(2003). Authigenic Minerals and Diagenesis in The Clastic Sediments of The Ghar Formation South and Southeast Iraq.. Iraqi National Journal of Earth Science, 3(1), 1-21. doi: 10.33899/earth.2003.36680
Ali Al-Juboury; Jamal S. Al-Ghrear; Mohammad A. Al-Rubaii. "Authigenic Minerals and Diagenesis in The Clastic Sediments of The Ghar Formation South and Southeast Iraq.". Iraqi National Journal of Earth Science, 3, 1, 2003, 1-21. doi: 10.33899/earth.2003.36680
(2003). 'Authigenic Minerals and Diagenesis in The Clastic Sediments of The Ghar Formation South and Southeast Iraq.', Iraqi National Journal of Earth Science, 3(1), pp. 1-21. doi: 10.33899/earth.2003.36680
Authigenic Minerals and Diagenesis in The Clastic Sediments of The Ghar Formation South and Southeast Iraq.. Iraqi National Journal of Earth Science, 2003; 3(1): 1-21. doi: 10.33899/earth.2003.36680
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