RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 20, ES2007, doi:10.2205/2020ES000706, 2020

Figure 13. A) – Types of cements that are present in upper Triassic and lower Cretaceous sandstone reservoirs and their relationship with depth; B) – quartz overgrowth developed on the surfaces of the detrital quartz grains; C) – crystals and booklets of kaolinite filling the pore spaces; D) – dolomite developed and surrounded the quartz grains; E) – developed siderite in the sandstone; F) – anhydrite patches filling some of the pore spaces.

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Citation: Yousef Ibrahem, Vladimir P. Morozov, Mohammad El Kadi (2020), Influence and control of post-sedimentation changes on sandstone reservoirs quality, example, upper Triassic (Mulussa F reservoir), and lower Cretaceous (Rutbah reservoir), Euphrates graben, Syria, Russ. J. Earth Sci., 20, ES2007, doi:10.2205/2020ES000706.

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