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Physical Sciences and Mathematics Commons

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Earth Sciences

TÜBİTAK

2020

Sequence stratigraphy

Articles 1 - 2 of 2

Full-Text Articles in Physical Sciences and Mathematics

Facies Distribution, Paleoenvironment And Sequence Stratigraphy Model Of The Oligo-Miocene Asmari Formation (Fars Province, South Of Iran), Fereshteh Kamalifar, Mohsen Aleali, Vahid Ahamadi, Akram Mirzaiee Jan 2020

Facies Distribution, Paleoenvironment And Sequence Stratigraphy Model Of The Oligo-Miocene Asmari Formation (Fars Province, South Of Iran), Fereshteh Kamalifar, Mohsen Aleali, Vahid Ahamadi, Akram Mirzaiee

Turkish Journal of Earth Sciences

The Oligocene (Rupelian-Chattian) to Miocene (Aquitanian)-aged Asmari Formation is considered one of the most significant petroliferous reservoirs in the Middle East. The Oligocene-Miocene Asmari Formation represents diverse facies patterns in different parts of Zagros, so analysis of its facies in different provinces of the Zagros Basin is necessary. In this study, the sedimentary depositional sequences of Asmari Formation in the Firuzabad (south of Shiraz) and Bastak (west of Bandar-Abbas) sections in the Zagros Basin (Fras Platform) have been analyzed for distinguishing facies characteristics, interpreting the paleoenvironment and determining dominant depositional sequences. Based on field investigations and laboratory studies, 13 microfacies …


Depositional Environment And Sequence Stratigraphy Of The Khoshyeilagh Formation Inbojnourd And Jajarm (Ne Iran), Fatemeh Jafarbeigloo, Mahmoud Reza Majidifard, Bahaeddin Hamdi, Afshin Asghari, Mehran Arian Jan 2020

Depositional Environment And Sequence Stratigraphy Of The Khoshyeilagh Formation Inbojnourd And Jajarm (Ne Iran), Fatemeh Jafarbeigloo, Mahmoud Reza Majidifard, Bahaeddin Hamdi, Afshin Asghari, Mehran Arian

Turkish Journal of Earth Sciences

In this study, depositional environment and sequence stratigraphy of the Khoshyeilagh Formation has been investigated in three stratigraphic sections including Pelmis, Robat-e Qarehbil, and Kuhe Ozon in the northeast of Iran. The thickness of the Khoshyeilagh Formation in these sections are 182, 260, and 463 m, respectively. Based on the facies analysis of the Khoshyeilagh Formation, 3 clastic facies, 11 carbonate facies, and 1 hybrid facies were identified. The vertical and lateral changes of the Khoshyeilagh Formation show a shoreface marine depositional environment that begins with alluvial sediments and continues by marine sedimentation. According to these changes, a homoclinal ramp …