Microfacies and stable isotope analysis of Kuldhar Member Limestone (Callovian–Oxfordian), Jaisalmer Basin, western Rajasthan: implications for depositional environment and diagenetic evolution
Microfacies, diagenesis, and stable isotope analysis of Kuldhar Member Limestone (KML) has been carried out to reconstruct the depositional environment and palaeogeography as well as to evaluate the influence of diagenesis on its reservoir quality. The KML is characterized by thin bedding, a high ab...
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Veröffentlicht in: | Carbonates and evaporites 2023-12, Vol.38 (4), p.81, Article 81 |
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