Abstract The Fujairah basin in the Gulf of Oman experienced a complex tectonic evolution related to Late Cretaceous ophiolite obduction and Oligocene‐Miocene Zagros continental collision. The structure of the foreland basin in Oman‐UAE is well‐known, but the structure and evolution of the hinterland basin behind the obducted ophiolite and underlying ...
M. Y. Ali +5 more
wiley +1 more source
Abstract The Late Cretaceous obduction of the Semail Ophiolite onto the rifted passive Arabian margin and the Cenozoic collisional tectonics with the final closure of the Neo‐Tethys Ocean, are major contributors to the present‐day crustal architecture of the northern United Arab Emirates (UAE). We acquired the first 3D grid magnetotelluric observations
B. A. Cherkose +5 more
wiley +1 more source
Study and Statistical Analysis of Geochemical Relations Active Elements in Sedimentary Phosphate Layers of Kuh-e- Lar Zagros-Anticline [PDF]
In this research, the layers of the sedimentary environment of the Pabdeh formation, which have different variation amounts of phosphate minerals (Apatite), were studied.
FARID BOLOURCHIFARD +3 more
doaj +1 more source
Impact of the Paleocene–Eocene Thermal Maximum (PETM) on organic petrographic characteristics of the basal Pabdeh Formation at Kuh-e-Gurpi Anticline, SW Iran [PDF]
This study investigates the impact of the Paleocene–Eocene Thermal Maximum (PETM) event on the organic petrographic characteristics of the base Pabdeh Formation in the Tang-e-Hati section, located at the Kuh-e-Gurpi Anticline, SW Iran.
Sasan Bakhtiary Nejad +2 more
doaj +1 more source
Microbiostratigraphy of the Jahrum Formation in Nimbashi section, West Estahban, Fars [PDF]
Introduction: Zagros sedimentary basin in the south and southwest of Iran holds oil and gas huge reservoirs. This basin which bordered the closure of the Paleotethys ocean (Berberian and King 1981), with high thickness of sedimentary sequences laid down
Reza Sadeghi, Maryam Jokar
doaj +1 more source
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]
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
Potential Evaluation and Basin Modeling of the Pabdeh Formation in Zagros Basin: A Case Study
Pabdeh Formation is one of the most important source rocks in Zagros basin. In this study, thermal modeling and comparing of hydrocarbon potential evaluation of Pabdeh Formation in Mish Anticline and Gachsaran oil field have been investigated. For this reason, Rock-Eval pyrolysis was carried out on 21 cuttings samples collected from 2 boreholes (Well ...
openaire +2 more sources
Depositional environment and sequence stratigraphy of the Asmari Formation in Kuh-e Asmari and Kuh-e Gurpi surface sections [PDF]
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
doaj
Stratigraphy and Sedimentary environment of Asmari Formation in Moshkan section, South east Yasuj [PDF]
: 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
doaj +1 more source
Biostratigraphy of the Gurpi Formation in Chenareh section based on calcareous nannofossils [PDF]
The 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
doaj +1 more source

