Muddy and dolomitic rip-up clasts in Triassic fluvial sandstones: Origin and impact on potential reservoir properties (Argana Basin, Morocco)
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文摘

Rip-up clasts may represent a significant part of host sandstone framework.

Spatial distribution of these grains is strongly facies-related.

There are three different types according to their composition and ductility.

They are important sources of information for paleogegraphic reconstructions.

Their occurrence is a key factor on diagenetic evolution and reservoir quality.

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