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Depositional and Diagenetic Facies in the Jurassic Arab-C and -D Reservoirs, Qatif Field, Saudi Arabia

  • Augustus O. Wilson
Part of the Casebooks in Earth Sciences book series (CASEBOOKS)

Abstract

Qatif Field is a giant oil field that straddles the northeastern Persian Gulf coast of Saudi Arabia (Fig. 20-1). ARAMCO discovered Qatif in early 1946, after surface geology and gravity surveys had indicated the presence of a major north—south anticlinal structure. Qatif is interpreted as a low-amplitude, “banana-shaped” shear fold, convex westward (Fig. 20-2), which was probably formed by right-lateral displacement along basement faults, and possibly enhanced by deep movement of salt from the Cambrian Hormuz Salt. The structure lies on the eastern side of the Arabian Plate, but well to the west of the intense Zagros Mountains fold belt near the plate boundary in Iran.

Keywords

Saudi Arabia Reservoir Rock Carbonate Facies Lime Mudstone Reservoir Facies 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer-Verlag New York Inc. 1985

Authors and Affiliations

  • Augustus O. Wilson

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