Landslide damming: implications for natural hazards and risks [PDF]
, 2020 Understanding the landslide debris emplacement kinematics and the landslide failure mechanisms is essential for the definition of hazard and for the reconstruction of risk scenarios functional to mitigation strategies. Landslides in the southwest of Iran
ROUHI, JAVAD
core
A seismic-driven 3D model of rock mechanical facies: An example from the Asmari reservoir, SW Iran [PDF]
, 2016 Asmari Formation is one of the most prolific and important hydrocarbon reservoirs in Iran. This formation in the Cheshmeh-Khosh oilfield shows mixed carbonate-siliciclastic lithology and its elastic modulus changes are correlatable with facies changes ...
Gharechelou, S. +5 more
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Regional stratigraphy, facies distribution, and hydrocarbons potential of the Oligocene strata across the Arabian Plate and Western Iran [PDF]
, 2019 Major global events during the Oligocene epoch included a climatic change from warm “greenhouse” to a cooler “icehouse” that was accompanied by the onset of Antarctic glaciation. These events led to decline in water temperature, salinity, nutrient supply
Alsharhan A.S., Sadooni F.N.
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Tectonic controls on residual oil saturation below the present-day fluid contact level in reservoirs of the Persian Gulf [PDF]
, 2020 Acknowledgments The authors would like to acknowledge, and gratefully appreciate the support of, the Aberdeen Formation Evaluation Society for their sponsorship, and Emerson (Paradigm) for providing the Geology software for the development of this study ...
Alsop, G. I. +3 more
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The application of crude oil biomarker and non-biomarker compounds in the determination of migration pathways and filling points of the Asmari reservoir in an oil field from the NE of Dezful Embayment [PDF]
علوم زمین خوارزمی, 2023 Reconstruction of migration pathways and filling points in a field provides critical information about the location of the source kitchen and future exploration prospects in the study area.
Morteza Asemani, Zahra Gholami
doaj
Biostratigraphy of Early Oligocene - Early Miocene Asmari Formation at the Southern Flank of Mish Anticline, Izeh Zone, SW Iran [PDF]
, 2019 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 ...
Moghaddam, Maghfouri, Rashnow, H.
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Depositional environment and sequence stratigraphy of the Asmari Formation in Kuh-e Asmari and Kuh-e Gurpi surface sections [PDF]
Journal of Stratigraphy and Sedimentology Researches, 2016 In this research the sedimentary successions of the Asmari Formation with the age of Oligocene â Miocene in two outcrops of kuhâe Asmari, located in the Dezful embayment with a thickness of 349 m and kuhâe Gurpi (Pabdeh valley), located at the Izeh
Mahnaz Dehghanzadeh +4 more
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Stratigraphy and Sedimentary environment of Asmari Formation in Moshkan section, South east Yasuj [PDF]
Journal of Stratigraphy and Sedimentology Researches, 2015 : The present research studies sedimentary succession of Oligocene Asmari Formation at Tang-e Moshkan stratigraphic section aimed at evaluating lithostratigraphy, biostratigraphy and determining microfacies, microfacies class, sub-environments, and ...
reza sadeghi +2 more
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Bivariate landslide susceptibility analysis in the Lorestan Arc (Zagros Mountains, Iran) [PDF]
, 2021 Landslide susceptibility analysis based on the assessment of a quantitative relationship between multiple controlling factors and landslide occurrence is a consolidated approach for land-use planning in risk mitigation.
Delchiaro, MicheleDelchiaro +5 more
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Biostratigraphy of the Gurpi Formation in Chenareh section based on calcareous nannofossils [PDF]
Journal of Stratigraphy and Sedimentology ResearchesThe Gurpi Formation was measured and sampled in a stratigraphic section located on the northern limb of the Chenareh anticline to the north of Andimeshk. The thickness of the Gurpi Formation in this section is 288.5 meters and its lower boundary with the
Zeinab Bayat +2 more
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