Results 51 to 60 of about 207 (128)
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
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
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
In this study, the sediments of the Pabdeh Formation in the Tange Lendeh section, with a thickness of 58 meters, are composed of purple shales and argillaceous limestones with chert and gray marl layers. A total of 56 calcareous nannofossil species, belonging to 22 genera from 13 families, were recognized in this strata.
habibi, kiana +2 more
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
The planktonic foraminifera turnover across the Danian-Selandian boundary (early to late Paleocene, ~60 Ma) has been studied in the Kamestan anticline section. The studied interval span planktonic foraminifera zones P2-P3.
Nasrin Hadavandkhani, Abbas Sadeghi
core +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
Microfacies, depositional environment and carbonate association of the Asmari Formation in Tang-e-Gojestan [PDF]
The Asmari Formation was logged and sampled in the Tang-e-Gojestan stratigraphic section (Eshgar Anticline, Izeh Zone) to study microfacies, depositional environment and carbonate associations. The Asmari Formation with 298 m-thickness mainly consists of
Yadolah Ezampanah, Mohammad Goodarzi
doaj +1 more source

