Source provenance
Memon, F.H., Tunio, A.H., Memon, K.R., Mahesar, A.A. & Abbas, G. (2023). Unveiling the Diagenetic and Mineralogical Impact on the Carbonate Formation of the Indus Basin, Pakistan: Implications for Reservoir Characterization and Quality Assessment. Minerals, 13(12), 1474.
Cited by 1 unit (1 published) · 5 field-level citations · 1 revision note.
Chiltan Limestone as Middle Jurassic oolitic shelf carbonate and reservoir.
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Units citing this source
- EpochLithologyDepositional environmentGeological significancePlain summary
- Lithology: Composed of thick, massive-bedded, shoaling-upward carbonate cycles dominated by grainstone (locally oolitic); microfacies range from lime mudstone (MF1) through bioclastic peloidal packstone (MF2) to bioclastic ooidal grainstone (MF3). Laterite and karstification at the top record paleo-exposure that enhances reservoir quality (Iqbal et al. 2012; Memon et al. 2023).