2003
DOI: 10.1306/07080302021
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Pool characterization of Ordovician Midale field: Implication for Red River play in northern Williston basin, southeastern Saskatchewan, Canada

Abstract: Renhai Pu received a B.S. degree in petroleum geology from the Chengdu College of Geology (China) in 1983, an M.S. degree from the China University of Geosciences (Beijing) in 1990, and a Ph.D. from Northwest University (China) in 1998. He has been teaching seismic interpretation and sequence stratigraphy in Northwest University (China) for 13 years. His current research interests are in reservoir prediction and exploration of subtle traps.

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Cited by 16 publications
(8 citation statements)
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References 12 publications
(14 reference statements)
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“…Allen et al, 2010). Sedimentation was broadly affected by local as well as regional fault systems which were later reactivated at various times (Oglesby, 1987;Lefever et al, 1987;Greggs and Greggs, 1989;Gerhard et al, 1991;Pu et al, 2003;Dixon, 2008). In southeastern Saskatchewan the basement is thought to have been dissected by a series of lineaments or faults dominated by an orthogonal NW−SE and NE−SW orientation (Potter and St. Onge, 1991;Kreis and Kent, 2000;Nimegeers and Haidl, 2004).…”
Section: Herald Formation Lithologymentioning
confidence: 99%
“…Allen et al, 2010). Sedimentation was broadly affected by local as well as regional fault systems which were later reactivated at various times (Oglesby, 1987;Lefever et al, 1987;Greggs and Greggs, 1989;Gerhard et al, 1991;Pu et al, 2003;Dixon, 2008). In southeastern Saskatchewan the basement is thought to have been dissected by a series of lineaments or faults dominated by an orthogonal NW−SE and NE−SW orientation (Potter and St. Onge, 1991;Kreis and Kent, 2000;Nimegeers and Haidl, 2004).…”
Section: Herald Formation Lithologymentioning
confidence: 99%
“…The lower two-thirds of the Yeoman Formation lack sufficient porosity and permeability to be considered a good reservoir unit. The uppermost third, which is known as the Upper Yeoman, is strongly mottled, sufficiently porous and permeable to form good quality reservoirs (Kendall, 1976; Kreis and Kent, 2000; Pu et al., 2003). Furthermore, the thin, commonly laminated, organic-rich interbeds (kerogenite or kukersite) within the Upper Yeoman are identified as the main source of petroleum in Red River reservoirs throughout the Williston Basin (Derby and Kilpatrick, 1985).…”
Section: Methodsmentioning
confidence: 99%
“…The uppermost third of the Yeoman Formation or Upper Yeoman is strongly mottled, commonly porous, and permeable. These have resulted in relatively good reservoir properties [43,44]. The Upper Yeoman also contains widely distributed, commonly laminated, relatively thin organic-rich interbeds, which are known as kukersites.…”
Section: Geological Settingmentioning
confidence: 99%