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Iraqi National Journal of Earth Science

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Diagenetic Processes and Their Progression in The Rocks of Injana Formation, Borehole (KH8/9), NW Iraq.

    Thamer A. Aghwan Ahmad N. Al-Fattah

Iraqi National Journal of Earth Science, 2003, Volume 3, Issue 1, Pages 22-35
10.33899/earth.2003.36681

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Abstract

Several diagenetic phenomena have affected the sandstones of Injana Formation. These include: compaction, cementation (manifested by dominance of carbonate cement with minor silica, ferruginous, and gypsum cements), replacement, recrystallization which noticed by the transformation of micritic matrix and fragments to sparry calcite whereas the alteration appeared through change of feldspar to clay minerals. Most of these diagenetic phenomena are related to eodiagenesis and minor rule of mesodiagenesis (alteration and partial recrystallization and cementation ).
Keywords:
    Diagenetic Processes Injana NW Iraq
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(2003). Diagenetic Processes and Their Progression in The Rocks of Injana Formation, Borehole (KH8/9), NW Iraq.. Iraqi National Journal of Earth Science, 3(1), 22-35. doi: 10.33899/earth.2003.36681
Thamer A. Aghwan Ahmad N. Al-Fattah. " Diagenetic Processes and Their Progression in The Rocks of Injana Formation, Borehole (KH8/9), NW Iraq.". Iraqi National Journal of Earth Science, 3, 1, 2003, 22-35. doi: 10.33899/earth.2003.36681
(2003). ' Diagenetic Processes and Their Progression in The Rocks of Injana Formation, Borehole (KH8/9), NW Iraq.', Iraqi National Journal of Earth Science, 3(1), pp. 22-35. doi: 10.33899/earth.2003.36681
Diagenetic Processes and Their Progression in The Rocks of Injana Formation, Borehole (KH8/9), NW Iraq.. Iraqi National Journal of Earth Science, 2003; 3(1): 22-35. doi: 10.33899/earth.2003.36681
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