Building the Zagros collisional orogen: timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence
The Zagros Mountains are the result of the Arabia/Eurasia collision initiated at~ 35Ma as the
rifted Arabian lithosphere was underthrusted beneath the Iranian plate due to its negative …
rifted Arabian lithosphere was underthrusted beneath the Iranian plate due to its negative …
[PDF][PDF] Carbonate reservoir rocks at giant oil and gas fields in SW Iran and the adjacent offshore: a review of stratigraphic occurrence and poro-perm characteristics
B Esrafili-Dizaji, H Rahimpour-Bonab - Journal of Petroleum …, 2019 - academia.edu
More than 6000 exploration and appraisal wells have been drilled in SW Iran since the
discovery of Masjid-i Soleiman in May 1908, resulting in the discovery of 124 oilfields and 57 …
discovery of Masjid-i Soleiman in May 1908, resulting in the discovery of 124 oilfields and 57 …
Strontium isotope stratigraphy
JM McArthur - 2010 - pubs.geoscienceworld.org
Strontium Isotope Stratigraphy | Application of Modern Stratigraphic TechniquesTheory and
Case Histories | GeoScienceWorld Books | GeoScienceWorld Skip to Main Content …
Case Histories | GeoScienceWorld Books | GeoScienceWorld Skip to Main Content …
Regional stratigraphic architecture and reservoir types of the Oligo-Miocene deposits in the Dezful Embayment (Asmari and Pabdeh Formations) SW Iran
FSP Van Buchem, TL Allan, GV Laursen… - Geological Society …, 2010 - lyellcollection.org
A regional sequence stratigraphic model is proposed for the Oligo-Miocene Asmari and
Pabdeh Formations in the Dezful Embayment of SW Iran. The model is based on both new …
Pabdeh Formations in the Dezful Embayment of SW Iran. The model is based on both new …
Early Neogene foreland of the Zagros, implications for the initial closure of the Neo-Tethys and kinematics of crustal shortening
We study the transition from passive margin to foreland basin sedimentation now exposed in
the High Zagros belt to provide chronological constraints on the initial stage of Arabia …
the High Zagros belt to provide chronological constraints on the initial stage of Arabia …
Late Cretaceous–Paleocene formation of the proto–Zagros foreland basin, Lurestan Province, SW Iran
Late Cretaceous emplacement of ophiolitic-radiolaritic thrust sheets over the Arabian
passive margin was the first manifestation of the protracted closure of the Neotethys Ocean …
passive margin was the first manifestation of the protracted closure of the Neotethys Ocean …
The Asmari Formation revisited: changed stratigraphic allocation and new biozonation
GV Laursen, S Monibi, TL Allan, NAH Pickard… - Shiraz 2009-1st EAGE …, 2009 - earthdoc.org
The essential biostratigraphy of the Asmari Formation was outlined in the early 1950's and
thereby the only published record of the biostratigraphy before the Asmari Formation was …
thereby the only published record of the biostratigraphy before the Asmari Formation was …
[HTML][HTML] Oligocene-Miocene ramp system (Asmari Formation) in the NW of the Zagros basin, Iran: Microfacies, paleoenvironment and depositional sequence
H Vaziri-Moghaddam, A Seyrafian, A Taheri… - Revista mexicana de …, 2010 - scielo.org.mx
The Asmari Formation deposited in the Zagros foreland basin during the Oligocene-
Miocene. Four different measured sections were studied in this area in order to interpret the …
Miocene. Four different measured sections were studied in this area in order to interpret the …
Integrated petrophysical and microfacies analyses for a reservoir quality assessment of the Asmari Dolostone sequence in the Khesht Field, SW Iran
R Fallah-Bagtash, MH Adabi, BS Nabawy… - Journal of Asian Earth …, 2022 - Elsevier
Abstract The Asmari Formation is one of the most important prolific reservoirs along both
sides of the Persian Gulf. The present study aims to characterize the fractured dolomite of …
sides of the Persian Gulf. The present study aims to characterize the fractured dolomite of …
Magnetochronology of synorogenic Miocene foreland sediments in the Fars arc of the Zagros Folded Belt (SW Iran)
The timing of deformation in the northern Zagros Folded Belt is poorly constrained because
of the lack of an accurate absolute chronology of the syntectonic sedimentary sequences …
of the lack of an accurate absolute chronology of the syntectonic sedimentary sequences …