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[1]
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Microfacies analysis of the Palaeocene Lockhart limestone on the eastern margin of the Upper Indus Basin (Pakistan): Implications for the depositional environment and reservoir characteristics
The Depositional Record,
2023
DOI:10.1002/dep2.222
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[2]
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Configuration and Timing of Collision Between Arabia and Eurasia in the Zagros Collision Zone, Fars, Southern Iran
Tectonics,
2021
DOI:10.1029/2021TC006762
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[3]
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Using Stable Isotope Analysis (δD and δ18O) and Tracing Tests to Characterize the Regional Hydrogeological Characteristics of Kazeroon County, Iran
Water,
2020
DOI:10.3390/w12092487
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[4]
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Using Stable Isotope Analysis (δD and δ18O) and Tracing Tests to Characterize the Regional Hydrogeological Characteristics of Kazeroon County, Iran
Water,
2020
DOI:10.3390/w12092487
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[5]
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Middle Eocene larger benthic foraminifera from Egypt and their similarity to the southern tethyan provinces
Journal of African Earth Sciences,
2019
DOI:10.1016/j.jafrearsci.2019.02.001
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[6]
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Microfacies and depositional environment of Asmari formation in the Zeloi oil field, Zagros basin, south-west Iran
Carbonates and Evaporites,
2019
DOI:10.1007/s13146-019-00507-1
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[7]
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Late Paleocene to Early Eocene larger benthic foraminifera biozones and microfacies in Estahbanate area, Southwest of Iran with Thetyan biozones correlation
Carbonates and Evaporites,
2018
DOI:10.1007/s13146-018-0464-8
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[8]
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Biostratigraphy and paleoecology of Upper Paleocene to Lower Oligocene deposits in Southeast of the Hajiabad Area (Zagros Basin, SW Iran)
Arabian Journal of Geosciences,
2015
DOI:10.1007/s12517-015-1778-7
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[9]
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Petrography, Sedimentary Environments and Sequence Stratigraphy of Asmari Formation in Central Fars, Zagros, SW (Iran)
Open Journal of Geology,
2014
DOI:10.4236/ojg.2014.412050
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