2017
DOI: 10.1016/j.jafrearsci.2017.02.020
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Source, tectonic setting, and facies distribution of the Silurian Sharawra Formation, the Old Qusaiba village, central Saudi Arabia

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Cited by 5 publications
(3 citation statements)
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“…The Sharawra Formation was deposited in a lower to upper shoreface environment, with sediment sourced from the Arabian Shield. The maximum thickness of the Sharawra Formation at this locality is 27 m, and the unit thins in the SW direction (Abbas et al, 2017). The top of the outcrop is capped by a hard layer of calcareous duricrust.…”
Section: Location 6: Lower Silurian Shale Of the Qusaiba Formationmentioning
confidence: 86%
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“…The Sharawra Formation was deposited in a lower to upper shoreface environment, with sediment sourced from the Arabian Shield. The maximum thickness of the Sharawra Formation at this locality is 27 m, and the unit thins in the SW direction (Abbas et al, 2017). The top of the outcrop is capped by a hard layer of calcareous duricrust.…”
Section: Location 6: Lower Silurian Shale Of the Qusaiba Formationmentioning
confidence: 86%
“…Along the dirt track that leads to the top of the cliff above Old Qusaiba village, we see the transition to the overlying Sharawra Formation, which is comprised of fine to medium grained subarkosic sandstones interbedded with green claystones (Abbas et al, 2017). Although fine silt layers can be seen in the upper part of shale of the Qusaiba Formation, the boundary with the overlying Sharawra Formation is placed at the lowermost sandstone bed.…”
Section: Location 6: Lower Silurian Shale Of the Qusaiba Formationmentioning
confidence: 88%
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