Energy Science & EngineeringThe Pabdeh Formation (Paleocene‐Oligocene) is one of the hydrocarbon‐generating formations in the Zagros sedimentary basin. In this study, to evaluate its hydrocarbon potential and the distribution of organic matter maturity, samples were collected from ...
Yingchun Liu +3 more
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Biostratigraphy of the Pabdeh Formation in the Parsi Oil Field (Dezful Embayment, South-West Iran) [PDF]
Journal of Stratigraphy and Sedimentology Researches, 2021 In order to study biostratigraphy and the determination of biozonation in the Pabdeh Formation based on the new planktonic foraminifera biozonation in the Tethys region, one subsurface section in well 1 of the Parsi Oil Field was selected in the southern
Masume Sabokro +3 more
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Investigating bio-events and time expansion of Calcareous nannofossils in the upper part of the Gurpi Formation and lower part of the Pabdeh Formation, northwestern Shiraz [PDF]
Journal of Stratigraphy and Sedimentology Researches, 2020 In this study, calcareous nannofossils are investigated in the upper part of the Gurpi Formation and lower part of the Pabdeh Formation at the Par-e Nobar section located in the northwest of Shiraz. The thickness of the studied section is about 41 m. The
Saeedeh Senemari, Behzad Saeedi razavi
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Biostratigraphy of Foraminifera at The Upper Cretaceous and Lower Paleogene Strata in The Kuh-E Genu, Bandar Abbas City, Northwestern Persian Gulf, Southern Iran [PDF]
Journal of Sciences, Islamic Republic of Iran, 2022 The study area is located in Tang-e Bagh at Kuh-e Genu, approximately 69 km, northern Persian Gulf. The age relationships of Sarvak, Gurpi, and Pabdeh formations were unclear in the study area because of the low-resolution biostratigraphy. Therefore, 152
Nadia Farsi +3 more
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Biostratigraphy of the Oligocene deposits of Pabdeh Formation based on planktonic foraminifera in Bandar Abbas area [PDF]
Journal of Stratigraphy and Sedimentology Researches, 2020 In this research, the biostratigraphy of Oligocene deposits of the Pabdeh Formation in Bandar Abbas region is considered. For this purpose, the planktonic foraminifera was studied and identified.
Jahanbakhash Daneshian +2 more
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Calcareous nannofossils at the upper part of Gurpi Formation and the lower part of Pabdeh Formation at Arkavaz section, south east Ilam [PDF]
Journal of Stratigraphy and Sedimentology Researches, 2019 In this study the Paleocene sediments have been investigated at the upper part of Gurpi Formation and the lower part of Pabdeh Formation at Arkavaz section in southeast of Ilam.
Saeedeh Senemari
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Biostratigraphy of the Pabdeh Formation based on planktonic foraminifera in the Tang-e-Chogan section in Interior Fars, Zagros Basin [PDF]
Journal of Stratigraphy and Sedimentology Researches, 2023 The biostratigraphy of the marly-limestone Pabdeh Formation has been studied in a section located in the Interior Fars (folded Zagros). Five assemblage biozones of plankton foraminifera with Early Eocene to Late Eocene age were identified in the studied ...
Zahra Khaloasgari +2 more
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Earth and Space Science, Volume 10, Issue 12, December 2023., 2023 Abstract The United Arab Emirates (UAE), located in an arid climate zone with low rainfall, relies on shallow aquifers for freshwater. Understanding the depth and extent of such aquifers is crucial for meeting water supply needs. The UAE's hydrogeology is influenced by neighboring mountains in Oman.
H. Saibi +5 more
wiley +1 more source
Evaluation of Pabdeh/Asmari boundary based on calcareous nannofossil biostratigraphy at north eastern limb of Gurpi anticline, Khuzestan Province [PDF]
Journal of Stratigraphy and Sedimentology Researches, 2018 Introduction One of the most extensive Tertiary deposits is the marine strata of Pabdeh and Asmari Formations in Zagros, which was studied based on paleontology studies. Type section of Pabdeh Formation is located in Tang-e Pabdeh, North of Lali oilfield
Saeedeh Senemari
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Subsidence and Uplift History of the UAE and the Western Flank of the UAE‐Oman Mountain Range
Tectonics, Volume 42, Issue 10, October 2023., 2023 Abstract The western flank of the UAE‐Oman mountain range offers a unique geodynamic setting to study the development of a cratonic rift into a mature passive margin and its subsequent flexure under orogenic load. However, the geodynamic processes driving this evolution are not fully understood. In this study, seismic and biostratigraphic data from 283
M. A. Jabir +3 more
wiley +1 more source