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• W2417963965 abstract "Research Article| March 01, 2016 Reference Section for the Horn River Group and Definition of the Bell Creek Member, Hare Indian Formation in central Northwest Territories Leanne J. Pyle; Leanne J. Pyle VI Geoscience Services Ltd. 939 Benvenuto Avenue, Brentwood Bay, BC V8M 1J8 Search for other works by this author on: GSW Google Scholar Len P. Gal Len P. Gal Consultant, Courtenay, BC V9J 1T6 Search for other works by this author on: GSW Google Scholar Bulletin of Canadian Petroleum Geology (2016) 64 (1): 67–98. https://doi.org/10.2113/gscpgbull.64.1.67 Article history received: 19 May 2015 accepted: 15 Jan 2016 first online: 12 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Leanne J. Pyle, Len P. Gal; Reference Section for the Horn River Group and Definition of the Bell Creek Member, Hare Indian Formation in central Northwest Territories. Bulletin of Canadian Petroleum Geology 2016;; 64 (1): 67–98. doi: https://doi.org/10.2113/gscpgbull.64.1.67 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 Abstract A stratigraphically complete section, exposed along a tributary to the Mountain River in the Northwest Territories, provides a reference section for the Devonian Horn River Group (Hare Indian, Ramparts, and Canol formations). Detailed whole rock geochemical data and total organic carbon content variations are related to the lithostratigraphy, thus providing a standard for regional correlation. The name ‘Bell Creek Member’ is proposed for the upper part of the Hare Indian Formation known as the “grey shale member”, and is defined at the Mountain River section. This member is heterogeneous and consists of two lithofacies: 1) a green-grey, silty shale and limestone facies (Bell Creek Member, grey facies); and 2) a dark grey, silty shale and limestone facies (Bell Creek Member, dark facies). The dark grey facies is described from a reference section along the Carcajou River, and is distributed south of 65°N latitude. The Bell Creek Member is Givetian in age. 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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