Sequence stratigraphy study of the Dariyan Formation in the Gadvan and Zana sections in the northeast and northwest of Shiraz, Zagros Basin, SW Iran

2020 ◽  
Vol 35 (4) ◽  
Author(s):  
Masoud Abedpour ◽  
Massih Afghah ◽  
Mohammadsadegh Dehghanian
Keyword(s):  
Sequence Stratigraphy ◽  
Zagros Basin ◽  
Sw Iran

Biostratigraphy and Sequence Stratigraphy of the Gurpi Formation at Deh Dasht Area, Zagros Basin, SW Iran

2014 ◽  
Vol 88 (6) ◽  
pp. 1681-1695 ◽  
Author(s):  
Mahboobeh FEREYDOONPOUR ◽  
Hossein VAZIRI-MOGHADDAM ◽  
Azizollah TAHERI
Keyword(s):  
Sequence Stratigraphy ◽  
Zagros Basin ◽  
Sw Iran ◽  
Gurpi Formation

Sequence Stratigraphy of Pabdeh Formation in Dezful Embayment (Zagros Basin) SW Iran

2010 ◽  
Author(s):  
Mehdi Khoshnoodkia ◽  
Hassan Mohseni ◽  
Ihsan S. Al-Aasm
Keyword(s):  
Sequence Stratigraphy ◽  
Zagros Basin ◽  
Dezful Embayment ◽  
Sw Iran ◽  
Pabdeh Formation

Depositional environment, sequence stratigraphy and biostratigraphy of the Gurpi formation in Fars zone, Zagros Basin (SW Iran)

2020 ◽  
Vol 35 (3) ◽  
Author(s):  
Seyed Abdolkarim Gowhari ◽  
Vahid Ahmadi ◽  
Hamzeh Saroea ◽  
Koros Yazdgerdi
Keyword(s):  
Sequence Stratigraphy ◽  
Depositional Environment ◽  
Zagros Basin ◽  
Sw Iran ◽  
Gurpi Formation

New biostratigraphic observations of planktonic foraminifera and ammonites on the Aptian–Albian intrashelf succession, Zagros Basin, SW Iran

2021 ◽  
pp. 104996
Author(s):  
Javad Sharifi ◽  
Mohammad Vahidinia ◽  
Atsushi Ando ◽  
Mohammad Hossein Mahmudy-Gharaie
Keyword(s):  
Planktonic Foraminifera ◽  
Zagros Basin ◽  
Sw Iran

scholarly journals Bio-Sequence Stratigraphy of Asmari Formation in the Southeast of Norabad (Zagros Basin, SW Iran)

2021 ◽  
Author(s):  
Mohammadsadegh Dehghanian
Keyword(s):  
Sea Level ◽  
Sequence Stratigraphy ◽  
Carbonate Platform ◽  
Reservoir Rock ◽  
Dispersion Pattern ◽  
Asmari Formation ◽  
Level Curve ◽  
Zagros Basin ◽  
Lithostratigraphic Units ◽  
Global Sea Level

Abstract Asmari Formation is the thick sequence of carbonate sediment in the range of Oligocene-Miocene which is deposited in the foreland basins of the Zagros and is considered as the original and most famous reservoir rock of Zagros basin. To study of lithostratigraphic units and sequence stratigraphy of this Formation, the section in the southeast of Norabad was selected. Field study indicated that Asmari Formation possessed the thickness of 401.5m and included 9 lithostratigraphic units. According to the study of microfacies, Stacking pattern and identification of main sequence level, three depositional sequences including two-second order and one-third order sequence were recognized. The sea-level curve in the studied section indicated that it was correspondence to the global sea level curve. These facies deposited in five environmental sedimentations as follow Open Sea Shelf (Fore Barrier), Bar, Lagoon, Back bar shelf, and Shoal. The environment is part of a carbonate platform that has been formed on an open shelf. In addition, according to the Study of foraminifer dispersion pattern the range of Asmari Formation in Norabad was suggested to be Oligocene (Rupelian- Chattian) to lower Miocene (Aquitanian- Burdigalian).

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