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- W2048410163 abstract "The Upper Oxfordian to Lower Kimmeridgian Hanifa Formation was deposited in an intra-platform basin on the broad epeiric shallow-water carbonate platform that extended over much of the Middle East during the Mesozoic. The formation consists of organic-rich carbonate mudstones, bioturbated mudstones and sulphates. The organic-rich mudstones are considered to be one of the major hydrocarbon source rocks in the Middle East oil province. The correlation of sedimentary facies shows a hierarchical stacking pattern of transgressive-regressive depositional cycles within the Hanifa Formation. Since these cycles occur at a basin-wide scale, it is assumed that they are related to relative changes of sea level. The superimposed scales of cyclicity determine the occurrence of source rock and sulphates. Major source rock development occurs in transgressive-dominated cycles. Sulphates, on the other hand, are more common during periods of overall regression." @default.
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- W2048410163 date "1990-12-01" @default.
- W2048410163 modified "2023-10-14" @default.
- W2048410163 title "Depositional cycles and source rock development in an epeiric intra-platform basin: the Hanifa Formation of the Arabian peninsula" @default.
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- W2048410163 doi "https://doi.org/10.1016/0037-0738(90)90054-w" @default.
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