Results 31 to 40 of about 139 (106)
Biostratigraphy and Paleoecological Study of Pabdeh Formation in Interior Fars, Zagros Basin, Iran
Open Journal of Geology, 2014 The Zagros basin, which trends NW-SE, is covered by a sea during the Paleogene, resulting in deposition of the Pabdeh Formation in the deeper parts of the basin. The thickness of the Pabdeh Formation in Tang-e-Abolhayat is about 221 m and it consists of purple shale at the base, gray shale, marl and marly limestone with a few horizons of nodular ...
Manooseh P. Khavari Khorassani +3 more
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Microfacies and Sedimentary Environments of Gurpi and Pabdeh Formations in Southwest of Iran [PDF]
American Journal of Applied Sciences, 2009 Problem statement: The Upper Cretaceous Gurpi and lower Tertiary Pabdeh formations as units of folded Zagros Zone were studied in three different regions (Tang-e-Abolhiat, Tang-e-Zanjiran and Maharloo) in Fars Province, Iran. Approach: Gurpi formation consisted of thin to medium sized layers of gray marl and marlstone interbedded with thin layers of ...
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Investigating microfacies and sedimentary environment of the Shahbazan Formation in the Lorestan Basin [PDF]
Journal of Stratigraphy and Sedimentology Researches, 2023 The Shahbazan Formation is dated to the middle to late Eocene age, after the Pyrenean orogenic phase. Following the progression of seawater, it was deposited in the Lorestan subzone and the folded Zagros basin. The lithology of this formation is composed
Peiman Rajabi, Parniya Abdulniya
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An Assessment of Infiltration Models in the Surface Soil of Geological Formations in Aleshtar Watershed, the Province of Lorestan [PDF]
پژوهشهای آبخیزداری, 2021 Soil infiltration is one of the key processes in the design of irrigation systems, water resources management, soil conservation, and erosion control in watershed management.
Shokofeh Hasanvand +3 more
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Bioestratigrafia do Oligoceno Inferior-Mioceno Inferior da Formação Asmari, Flanco Sul do Anticlinal Mish, Zona Izeh, SW Irã [PDF]
Anuário do Instituto de Geociências, 2018 In this research, biostratigraphy related to the Asmari Formation at the southern flank of Mish anticline, Izeh Zone, is discussed. In the studied stratigraphic section, the Asmari Formation overlies the Pabdeh Formation and underlies Quaternary ...
I. Maghfouri Moghaddam, H. Rashnow
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Geochemical investigation of petroleum source rocks by using Rock- Eval data in the Agha-Jari oilfield [PDF]
Journal of Stratigraphy and Sedimentology Researches, 2015 In this study, 40 drilling cutting of the Pabdeh, Gurpi, kazhdumi and Gadvan Formations from the Agha-Jari Oilfield were analyzed by using Rock-Eval pyrolysis.
Behzad khani +4 more
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Journal of Applied Sciences and Environmental Management, 2015 Palynological investigation about 120 samples from 460m thick outcrop section of late Paleocene to early Oligocene of the Pabdeh Formation, southwestern in Iran yield 55 species of dinoflagellate results to defined 7 biozone.
JN Ali Akbar, GN Ebrahim
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Study of water-level fluctuations throughout the deposition of the Gurpi Formation based on palynological data in the west of Dehrolan, south of Ilam [PDF]
Journal of Stratigraphy and Sedimentology Researches, 2020 To analyze the sedimentary palaeoenvironment of the Gurpi Formation in Bisheh–Deraz section in south of Ilam, various factors including diversity and abundance of dinocysts, a ratio of Peridinioid to Gonyaulacoid (P/G) dinoflagellate cysts, palynofacies ...
Mahsa Amiri, Elahe Zarei
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AIMS Geosciences, 2020 Phosphate deposits in south-western Iran are part of the South Tethyan Phosphogenic Province, a huge carbonate-dominated strata that extends to the Middle East.
Armin Salsani +4 more
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Tectonics, Volume 44, Issue 10, October 2025.Abstract Inception of obduction is a rare phenomenon in the Wilson cycle and requires specific prerequisites to transfer relatively high‐density oceanic lithosphere over the less‐dense continental lithosphere. The world's famous Semail ophiolite belt developed during the Late Cretaceous, when Neo‐Tethyan oceanic lithosphere obducted onto the rifted ...
M. Ismaiel, M. Y. Ali, A. Decarlis
wiley +1 more source