Results 31 to 40 of about 3,997,362 (141)
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
Earth and Space Science, Volume 10, Issue 8, August 2023., 2023 Abstract Hormuz salt formation is considered the origin of the evaporated salt deposits in the Zagros and its ductile behavior has been known as the reason for the inhomogeneous deformation in the Zagros. However, our knowledge about this formation has been limited to the salt domes on the surface.
H. Kianimehr +3 more
wiley +1 more source
The Depositional Record, Volume 8, Issue 3, Page 1031-1054, September 2022., 2022 One hundred and forty‐four sections of shallow‐water carbonates, deposited between the Palaeocene and the Miocene, from the Levant to the Himalaya, have been investigated to analyse the quantitative distribution of carbonate facies and carbonate‐producing organisms.
Giovanni Coletti +6 more
wiley +1 more source
Tectono‐Stratigraphic Evolution of the Foreland Fold‐and‐Thrust Belt of the United Arab Emirates
Tectonics, Volume 41, Issue 9, September 2022., 2022 Abstract The subsurface and surface structural geometries of the United Arab Emirates (UAE) fold‐and‐thrust belt (FTB) and foreland basins are interpreted from seismic, well data, and surface geology. Twelve horizons ranging in age from Miocene to Lower Jurassic were interpreted and mapped.
A. Abdelmaksoud, M. Y. Ali, M. P. Searle
wiley +1 more source
Journal of Palaeogeography, 2021 Data obtained from the calcareous nannofossils, distributed in the upper part of the Pabdeh Formation (Priabonian–Rupelian) and the lower part of the Asmari Formation (Chattian) in the Bid-Zard section, were used to investigate the Eocene to Oligocene ...
Saeedeh Senemari, Farah Jalili
doaj +1 more source
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 ...
openaire +1 more source
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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Penser le métier par la formation [PDF]
, 2020 Cet ouvrage examine, à partir de chantiers empiriques, les questions posées par la conception des dispositifs au long de parcours de formation professionnelle. Il s’adresse au monde de la recherche, mais aussi aux étudiant·e·s, aux praticien·ne· s engagé·
Charlier, Evelyne +3 more
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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
doaj +1 more source