Stress and Fracture Prediction with Geomechanical Reservoir Models – Concepts and Case Study, Eastern Sirte Basin

Author(s):  
A. Henk ◽  
A. Frischbutter
2012 ◽  
Author(s):  
Shahab D. Mohaghegh ◽  
Jim S. Liu ◽  
Razi Gaskari ◽  
Mohammad Maysami ◽  
Olugbenga A. Olukoko

2003 ◽  
Author(s):  
Harun Ates ◽  
Asnul Bahar ◽  
Salem El-Abd ◽  
Mohsen Charfeddine ◽  
Mohan Kelkar ◽  
...  

2011 ◽  
Author(s):  
Liu Haijun ◽  
Ling Yun ◽  
Guo Xiangyu ◽  
Guo Jun ◽  
Sun Desheng

2018 ◽  
Author(s):  
Taiwen Chen ◽  
Mohamed Hafez ◽  
Alaa Moustafa ◽  
Hanan Al-Hasan ◽  
Fatma Basha ◽  
...  

2000 ◽  
Author(s):  
J. Ashbridge ◽  
C. Pryce ◽  
F. Coutel ◽  
M. Welch ◽  
M. Ashton

2021 ◽  
Vol 61 (2) ◽  
pp. 720
Author(s):  
Kasia Sobczak ◽  
Heinz-Gerd Holl ◽  
Andrew Garnett

The Upper Jurassic Walloon Coal Measures of the Surat Basin (Queensland) host some of the most prominent coal seam gas (CSG) resources in Australia. The Walloon Coal Measures are directly overlain by the Springbok Sandstone formation, historically referred to as a regional aquifer. An increasing number of studies and industry models suggest relatively limited hydraulic connectivity within the formation and between it and the underlying coal measures, due to extreme lithological heterogeneity. Accurate evaluation of the permeability, as well as lateral and vertical continuity of the lithological units within the Springbok Sandstone, is critical in reservoir models that form the basis of reasonable aquifer protection practices and impact prediction. This study presents a wireline log-based workflow applied to identify permeable zones within the Springbok Sandstone in 31 CSG wells across the Surat Basin that allows robust estimations of porosities and Klinkenberg permeabilities. The workflow primarily utilises spontaneous potential, density, neutron and resistivity logs, and was developed by integrating current industry practices implemented by operators on a local scale to identify risk (permeable) zones in the vicinity of targeted coal seams. The results of this case study indicate that permeable zones within the interval are volumetrically minor (on average 25% N/G) and likely isolated, with Klinkenberg permeabilities rarely exceeding 10–20mD. This evidence for low hydraulic connectivity, as well as significant local variations in the character of the Springbok Sandstone, suggests that the definition of the formation as a regional, continuous aquifer and the way it is modelled needs to be revised.


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