Organic petrography and geochemistry of the Pabdeh Formation in Khaviz and Mansourabad anticlines, SW Iran [PDF]
This paper presents the results from organic geochemical evaluation of the Paleocene–Eocene Pabdeh Formation in the Khaviz Anticline and Mansourabad Oilfield by a combination of Rock-Eval pyrolysis method and organic petrographic techniques.
Marziyeh Khazami, Majid Alipour
doaj +2 more sources
Paleocene-Oligocene dinoflagellate cysts from the Siah Anticline, Zagros Basin, Southwest Iran [PDF]
A section of the Pabdeh Formation dating back to the Paleocene-Oligocene has been sampled in the Zagros Basin in Southwest Iran for palynological investigations and evaluation of thermal maturity and hydrocarbon generation potential.
Ali Akbar Jafar Nezhad +1 more
doaj +3 more sources
Reappraisal of lithology and depositional environment of carbonate-siliciclastic succession of the Pabdeh Formation in SE Ilam Province, W Iran [PDF]
The Pabdeh Formation (Paleocene–Oligocene) is located in the Zagros foreland basin. This formation was well appreciated as a source rock and somehow a potential reservoir particularly in the Dezful Embayment.
Seyedeh Zahra Hoseini Asgarabadi +3 more
doaj +2 more sources
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 +4 more sources
Bioestratigrafia do Oligoceno Inferior-Mioceno Inferior da Formação Asmari, Flanco Sul do Anticlinal Mish, Zona Izeh, SW Irã [PDF]
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 +4 more sources
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 +3 more sources
THE DEEP-SEA HATCHETFISH ARGYROPELECUS (STERNOPTYCHIDAE) IN THE EOCENE OF IRAN: DESCRIPTION AND PHYLOGENETIC RELATIONSHIPS OF TWO NEW SPECIES FROM THE PABDEH FORMATION [PDF]
Two new deep-sea hatchetfish species, †Argyropelecus iranicus n. sp. and †Argyropelecus zagrosensis n. sp., are described in detail herein based on fossil material from the Eocene (Bartonian) deposits of the Pabdeh Formation, Zagros Basin, Iran.
lorenzo ridolfi +5 more
doaj +2 more sources
Chemical Variation during Pabdeh Formation Deposition, Zagros Basin: Gurpi-Pabdeh-Asmari Boundaries determination and Paleoenvironmental Condition [PDF]
Determination of the formation of the Pabdeh boundary is a main challenge in Zagros sedimentary basin area. The work on hand is an attempt to clarify those based on chemical changes. The location under observation is the outcrop of the Pabdeh Formation (Paleocene-Oligocene) in Bangestan Anticline, the southern part of Zagros orogenic belt.
Tabatabaei Hossein Motamed Ahmad +1 more
openaire +1 more source
Abstract The United Arab Emirates (UAE), located in an arid climate zone with low rainfall, relies on shallow aquifers for freshwater. Understanding the depth and extent of such aquifers is crucial for meeting water supply needs. The UAE's hydrogeology is influenced by neighboring mountains in Oman.
H. Saibi +5 more
wiley +1 more source
Subsidence and Uplift History of the UAE and the Western Flank of the UAE‐Oman Mountain Range
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

