2020
DOI: 10.1016/j.marpetgeo.2019.05.001
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Sedimentology, geochemistry and reservoir potential of the organic-rich Qusaiba Shale, Tabuk Basin, NW Saudi Arabia

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Cited by 25 publications
(3 citation statements)
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“…Moreover, the Mg/Ca, K 2 O + NaO, and G/C 31 H parameters are effective indicators of the change of the paleosalinity. 59,61,62 As shown in Figure 12, the change of the paleosalinity is consistent with the evolution the depositional environment. 4.2.…”
Section: Resultssupporting
confidence: 76%
See 1 more Smart Citation
“…Moreover, the Mg/Ca, K 2 O + NaO, and G/C 31 H parameters are effective indicators of the change of the paleosalinity. 59,61,62 As shown in Figure 12, the change of the paleosalinity is consistent with the evolution the depositional environment. 4.2.…”
Section: Resultssupporting
confidence: 76%
“…The mudstone, bioclastic limestone, and limestone samples of P 1–2 g–q and C 3 c show high Sr/Ba and log­(MgO/Al 2 O 3 ) values, but the Th/U and V/Ni values are relatively low, indicating that the source rocks of P 1–2 g–q and C 3 c were deposited in a marine environment (Figure ). Moreover, the Mg/Ca, K 2 O + NaO, and G/C 31 H parameters are effective indicators of the change of the paleosalinity. ,, As shown in Figure , the change of the paleosalinity is consistent with the evolution the depositional environment.…”
Section: Resultsmentioning
confidence: 77%
“…It can be produced from both marine and lacustrine shales. Marine shale is generally developed in a stable and gentle tectonic environment, has a few types of lithofacies (Loucks and Ruppel, 2007;Abouelresh et al, 2020), and is widely distributed . In comparison, lacustrine shale formed in a continental rift basin has various types of lithofacies owing to paleogeological conditions such as a relatively small lake area, multiple material sources, and frequent climate changes (Wang et al, 2016;Jia et al, 2018;Li et al, 2020).…”
Section: Introductionmentioning
confidence: 99%