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• W2010191555 abstract "Other| December 01, 2000 Reply to Discussion: Vreeland Diamictites - Neoproterozoic glaciogenic slope deposits, Rocky Mountains, northeast British Columbia* M.E. McMechan M.E. McMechan Geological Survey of Canada, 3303 - 33 Street NW, Calgary, AB, T2L 2A7 Search for other works by this author on: GSW Google Scholar Author and Article Information M.E. McMechan Geological Survey of Canada, 3303 - 33 Street NW, Calgary, AB, T2L 2A7 Publisher: Canadian Society of Petroleum Geologists Received: 06 Nov 2000 Accepted: 10 Nov 2000 First Online: 02 Mar 2017 Online ISSN: 2368-0261 Print ISSN: 0007-4802 © The Society of Canadian Petroleum Geologists Bulletin of Canadian Petroleum Geology (2000) 48 (4): 364–366. https://doi.org/10.2113/48.4.364 Article history Received: 06 Nov 2000 Accepted: 10 Nov 2000 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation M.E. McMechan; Reply to Discussion: Vreeland Diamictites - Neoproterozoic glaciogenic slope deposits, Rocky Mountains, northeast British Columbia. Bulletin of Canadian Petroleum Geology 2000;; 48 (4): 364–366. doi: https://doi.org/10.2113/48.4.364 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 SocietyBulletin of Canadian Petroleum Geology Search Advanced Search Hoffman et al.(1998b) developed a modified ‘snowball’ Earth hypothesis to explain the association of Neoproterozoic low-latitude glaciation with the deposition of “cap carbonate” rocks bearing highly depleted carbon isotopic values. According to this hypothesis, a runaway albedo feedback caused the world’s oceans to freeze for millions of years. During this time interval, the continental ice cover was thought to have become thin and patchy because of the virtual elimination of the hydrological cycle (Kirschvink, 1992; Hoffman et al., 1998b). The Vreeland diamictites record vigorous erosion by an extensive ice sheet at or near the pressure melting... 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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• W2010191555 title "Reply to Discussion: Vreeland Diamictites - Neoproterozoic glaciogenic slope deposits, Rocky Mountains, northeast British Columbia" @default.
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