Microfacies and stable isotope analysis of Kuldhar Member Limestone (Callovian–Oxfordian), Jaisalmer Basin, western Rajasthan: implications for depositional environment and diagenetic evolution
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
https://link.springer.com/content/pdf/10.1007/s13146-023-00905-6.pdf
Reference91 articles.
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2. Adabi MH (2009) Multistage dolomitization of upper Jurassic mozduran formation, Kopet-Dagh Basin, ne Iran. Carb Evap 24:16–32. https://doi.org/10.1007/BF03228054
3. Ahmad AHM, Bhat GM, Khan MH (2006) Depositional environments and diagenesis of the kuldhar and Keera Dome carbonates (Late Bathonian-Early Callovian) of Western India. J Asian Earth Sci 27:765–778. https://doi.org/10.1016/j.jseaes.2005.06.013
4. Ahmad F, Quasim MA, Ahmad AHM (2021) Microfacies and diagenetic overprints in the limestones of Middle Jurassic Fort Member (Jaisalmer Formation), Western Rajasthan, India: Implications for the depositional environment, cyclicity, and reservoir quality. Geol J 56:130–151. https://doi.org/10.1002/gj.3945
5. Ahr WM (1973) The carbonate ramp: an alternative to the shelf model: transactions of the Gulf Coast Association of Geological Societies, v. 23
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