Sequence Stratigraphy and Chemostratigraphy Interpretations Based on Stable Isotope and Gamma Ray: An Example from the Early Triassic Lower Mahil Formation [Upper Khuff Outcrop Equivalent (KS1)], al Jabal Al-Akhdar, North Oman, Sultanate of Oman

Author:

Moustafa Mohamed S. H.,El-Ghali Mohamed A. K.,Al Raqaishi Rasha,Abbasi Iftikhar Ahmed,Al-Awah Hezam,Farfour Mohammed,Al Ghafri Nada,Al Humaidi Aaraf

Publisher

Springer Nature Switzerland

Reference8 articles.

1. Alsharhan, A. (2006). Sedimentological character and hydrocarbon parameters of the middle Permian to early Triassic Khuff formation. United Arab Emirates. Sedimentary Geology, 11(1–4), 121–156.

2. Forbes, G.A., Jansen, H. S. M., & Schreurs, J. (2010). Lexicon of Oman subsurface stratigraphy: Reference guide to the stratigraphy of Oman's hydrocarbon basins. GeoArabia Special Publication 5, Gulf PetroLink, Bahrain, p 371.

3. Goldhammer, R. K., Dunn, P. A., Hardie, L. A. (1990). Depositional cycles, composite sea-level changes, cycle stacking patterns, and the hierarchy of stratigraphic forcing: examples from Alpine Triassic platform carbonates.Geological Society of America Bulletin 102(5), 535–562.

4. Gradstein F. M., et al., (2012). (Eds). The geologic time scale 2012. Elsevier.

5. Koehrer, B., Aigner, T., Forke, H., & Pöppelreiter, M. (2012). Middle to upper Khuff (Sequences KS1 to KS4) outcrop-equivalents in the Oman Mountains. Grainstone architecture on a subregional scale, GeoArabia,59–104.

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