Re-evaluating the Paleogeography of the River-dominated and Wave-influenced Ferron Notom Delta, Southern Central Utah: an Integration of Detailed Facies-architecture and Paleocurrent Analysis

2018 ◽  
Vol 88 (2) ◽  
pp. 214-240 ◽  
Author(s):  
Yangyang Li ◽  
Janok P. Bhattacharya ◽  
Sumiyyah Ahmed ◽  
Daniel Garza
Keyword(s):  
Facies Architecture ◽  
Southern Central ◽  
Paleocurrent Analysis

Forward Stratigraphic Modeling of Kuwait Formation, Linking Facies Architecture to Hydrocarbon Occurrence

2021 ◽  
Author(s):  
Aimen Amer ◽  
Ali Gadalla Najem ◽  
Mubarak Al-Hajeri ◽  
Sergio Courtade ◽  
Per Salomonsen
Keyword(s):  
Model Simulation ◽  
Wave Activity ◽  
Sediment Supply ◽  
Facies Architecture ◽  
Facies Distribution ◽  
Accommodation Space ◽  
Stratigraphic Model ◽  
Main Driver ◽  
Kuwait Group ◽  
Paleocurrent Analysis

Abstract The objective of this study is to perform forward stratigraphic modeling on the Kuwait Formation (also known as Kuwait Group) exposed stratigraphic succession along the Jal Az-Zor escarpment to explain the enigmatic occurrence of an elongated NW-SE geobody mapped from subsurface data at northern Kuwait. Outcrop measurements such as; stratigraphic successions, facies distribution, critical facies trends, and paleocurrent analysis have been collected along the 60 km length of the Jal Az-Zor escarpment. Such measurements were combined with thin section lab analysis to reveal the various sedimentary processes such as wave activity, grain size distribution, sediment supply sources, accommodation space, and erosional rates. These measurements were combined with subsurface data such as seismic attributes to reconstruct the paleography of the area and run a forward stratigraphic model simulation. The vertical succession was also utilized to reconstruct the relative sea-level fluctuation through time to develop an accurate model. Forward stratigraphic modeling resulted in building a robust and reliable facies distribution 3D model for the Jal Az-Zor escarpment that demonstrates the complex facies architecture. The model shows the various stacking patterns of several depositional sequences that are observed in the field as well as the subsurface. The enigmatic geobody mapped from seismic as a channel system in previous publications turned out to be a paleoshoreline. This shoreline is composed of high-quality sands as a result of an elevated level of wave activity. Reworking of barrier island sands was also found to be responsible for the enhanced reservoir quality. Consequently, regardless of the subsurface structure, the main driver of successful hydrocarbon accumulation is directly linked to the NW-SE trending paleoshoreline. To the best of the authors’ knowledge, this is the first time forward-stratigraphic modeling is performed along the Jal Az-Zor escarpment in north Kuwait and using such an approach to unravel Kuwait Formation heavy hydrocarbon subsurface occurrences.

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