Cyclostratigraphy of the Lower Triassic Kangan Formation in the Salman gas field, eastern Persian Gulf, Iran

2021 ◽  
Vol 561 ◽  
pp. 110045
Author(s):  
Omid Falahatkhah ◽  
Ali Kadkhodaie ◽  
Ali Asghar Ciabeghodsi ◽  
Mingsong Li
2017 ◽  
Vol 10 (12) ◽  
Author(s):  
Ali-Akbar Irajian ◽  
Kamaladdin Bazargani-Guilani ◽  
Rahim Mahari ◽  
Ali Solgi ◽  
Alireza Moshrefizadeh ◽  
...  

2019 ◽  
Vol 164 ◽  
pp. 1-10 ◽  
Author(s):  
Mohammad Ali Faraji ◽  
Ali Kadkhodaie ◽  
David A. Wood ◽  
Hossain Rahimpour-Bonab ◽  
Mandana Ghanavati

2014 ◽  
Vol 30 (1) ◽  
pp. 25-43 ◽  
Author(s):  
Maryam Peyravi ◽  
Hossain Rahimpour-Bonab ◽  
Fadi H. Nader ◽  
Mohammad Reza Kamali

1971 ◽  
Vol 11 (1) ◽  
pp. 59
Author(s):  
P. Hosemann

The Basal Triassic Sandstone is the basal member of the Lower Triassic Kockatea Shale. It is widely distributed adjacent to, and on the Precambrian Greenough Block in the northern Perth Basin, Western Australia. This member is lowermost Lower Triassic in age in the subsurface of the Don-gara gas field. In outcrop on the Greenough Block, the member is represented by a thin basal conglomerate, conformably overlain by upper Lower Triassic Kockatea Shale. In this stratigraphic study, detailed well-to-well correlations and lithologic studies were integrated to reconstruct the depositional history of the interval encompassing the Basal Triassic Sandstone. This sandstone is a composite of near-shore marine, and strand line accumulations deposited around the flanks and on the Greenough Block during a Lower Triassic marine transgression. The sandstone bodies were deposited on a drowned, topography of low relief, on progressively truncated Permian formations and Precambrian basement. The topography was formed following uplift and tilting of the Greenough Block and the overlying Lower Permian formations during mild Upper Permian tectonism.


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