Sequence stratigraphy of Cenomanian–Turonian carbonate platform margins (Sarvak Formation) in the High Zagros, SW Iran: an outcrop reference model for the Arabian Plate

2010 ◽  
Vol 329 (1) ◽  
pp. 187-218 ◽  
Author(s):  
P. Razin ◽  
F. Taati ◽  
F. S. P. van Buchem
Keyword(s):  
Sequence Stratigraphy ◽  
Reference Model ◽  
Carbonate Platform ◽  
Arabian Plate ◽  
Sarvak Formation ◽  
Sw Iran

Depositional environments and sequence stratigraphy of the Sarvak Formation in an oil field in the Abadan Plain, SW Iran

Facies ◽  
2016 ◽  
Vol 62 (4) ◽  
Author(s):  
Ali Assadi ◽  
Javad Honarmand ◽  
Seyed-Ali Moallemi ◽  
Iraj Abdollahie-Fard
Keyword(s):  
Sequence Stratigraphy ◽  
Depositional Environments ◽  
Oil Field ◽  
Sarvak Formation ◽  
Sw Iran

Reservoir zonation in the framework of sequence stratigraphy: A case study from Sarvak Formation, Abadan Plain, SW Iran

2021 ◽  
pp. 109560
Author(s):  
Arad Kiani ◽  
Mohammad Hossein Saberi ◽  
Bahman ZareNezhad ◽  
Elham Asadi Mehmandosti
Keyword(s):  
Sequence Stratigraphy ◽  
Sarvak Formation ◽  
Reservoir Zonation ◽  
Sw Iran

A Cenomanian–Santonian rudist–bearing carbonate platform on the northern Arabian Plate, Turkey: facies and sequence stratigraphy

2020 ◽  
Vol 110 ◽  
pp. 104414 ◽  
Author(s):  
Oğuz Mülayim ◽  
İsmail Ömer Yılmaz ◽  
Sacit Özer ◽  
Bilal Sarı ◽  
Kemal Taslı
Keyword(s):  
Sequence Stratigraphy ◽  
Carbonate Platform ◽  
Arabian Plate

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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