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• W2083098768 abstract "Research Article| July 01, 2000 Reversal of the regional-scale flow system of the Williston basin in response to Pleistocene glaciation Stephen Grasby; Stephen Grasby 1Geological Survey of Canada, 3303 33rd Street N.W., Calgary, Alberta T2L 2A7, Canada Search for other works by this author on: GSW Google Scholar Kirk Osadetz; Kirk Osadetz 1Geological Survey of Canada, 3303 33rd Street N.W., Calgary, Alberta T2L 2A7, Canada Search for other works by this author on: GSW Google Scholar Robert Betcher; Robert Betcher 2Water Resources Branch, Manitoba Natural Resources, Box 18, 200 Saulteaux Crescent, Winnipeg, Manitoba R3J 3W3, Canada Search for other works by this author on: GSW Google Scholar Frank Render Frank Render 2Water Resources Branch, Manitoba Natural Resources, Box 18, 200 Saulteaux Crescent, Winnipeg, Manitoba R3J 3W3, Canada Search for other works by this author on: GSW Google Scholar Author and Article Information Stephen Grasby 1Geological Survey of Canada, 3303 33rd Street N.W., Calgary, Alberta T2L 2A7, Canada Kirk Osadetz 1Geological Survey of Canada, 3303 33rd Street N.W., Calgary, Alberta T2L 2A7, Canada Robert Betcher 2Water Resources Branch, Manitoba Natural Resources, Box 18, 200 Saulteaux Crescent, Winnipeg, Manitoba R3J 3W3, Canada Frank Render 2Water Resources Branch, Manitoba Natural Resources, Box 18, 200 Saulteaux Crescent, Winnipeg, Manitoba R3J 3W3, Canada Publisher: Geological Society of America Received: 23 Dec 1999 Revision Received: 07 Apr 2000 Accepted: 18 Apr 2000 First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2000) 28 (7): 635–638. https://doi.org/10.1130/0091-7613(2000)28<635:ROTRFS>2.0.CO;2 Article history Received: 23 Dec 1999 Revision Received: 07 Apr 2000 Accepted: 18 Apr 2000 First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Stephen Grasby, Kirk Osadetz, Robert Betcher, Frank Render; Reversal of the regional-scale flow system of the Williston basin in response to Pleistocene glaciation. Geology 2000;; 28 (7): 635–638. doi: https://doi.org/10.1130/0091-7613(2000)28<635:ROTRFS>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Low δ18O values of formation waters, collapse structures related to salt dissolution, hydrodynamic blowout structures, and biodegradation of oils all suggest a significant influx of fresh water into the Williston basin along the outcrop belt in southern and central Manitoba during Pleistocene glaciation. The thickness of the continental ice sheet over Manitoba would have provided sufficient potentiometric drive to reverse the regional-scale flow system of the Williston basin. The dynamic nature of the flow system suggests that modern-day pressure distributions may not be good proxies for ancient petroleum migration pathways as is commonly assumed. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2083098768 title "Reversal of the regional-scale flow system of the Williston basin in response to Pleistocene glaciation" @default.
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