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• W2014605364 abstract "Research Article| November 01, 1985 Late Paleozoic conodonts from ribbon chert delineate imbricate thrusts within the Antler Formation of the Slide Mountain terrane, central British Columbia L. C. Struik; L. C. Struik 1Geological Survey of Canada, 100 West Pender Street, Vancouver, British Columbia V6B 1R8, Canada Search for other works by this author on: GSW Google Scholar M. J. Orchard M. J. Orchard 1Geological Survey of Canada, 100 West Pender Street, Vancouver, British Columbia V6B 1R8, Canada Search for other works by this author on: GSW Google Scholar Author and Article Information L. C. Struik 1Geological Survey of Canada, 100 West Pender Street, Vancouver, British Columbia V6B 1R8, Canada M. J. Orchard 1Geological Survey of Canada, 100 West Pender Street, Vancouver, British Columbia V6B 1R8, Canada Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1985) 13 (11): 794–798. https://doi.org/10.1130/0091-7613(1985)13<794:LPCFRC>2.0.CO;2 Article history First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation L. C. Struik, M. J. Orchard; Late Paleozoic conodonts from ribbon chert delineate imbricate thrusts within the Antler Formation of the Slide Mountain terrane, central British Columbia. Geology 1985;; 13 (11): 794–798. doi: https://doi.org/10.1130/0091-7613(1985)13<794:LPCFRC>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 Late Devonian?–early Carboniferous to Permian conodonts from the Antler Formation of Slide Mountain Group near Barkerville, British Columbia, were extracted from 23 of 28 chert samples collected from a nearly continuous section on Sliding Mountain. The conodonts delineate three, possibly four, thrust sheets within the section. From bottom to top the ages recorded in the sheets consist of (I) Early Permian, (II) Pennsylvanian to Early Permian, (III) Early Mississippian to Early Permian, and (IV) Late Devonian? or Early Mississippian. In sheet III, 100 m.y. of chert and basalt stratigraphy, the entire known age span of the Antler Formation, is recorded in less than 300 m. Prior to thrust imbrication the Antler Formation must have been very thin and possibly covered a large area. Within individual thrust sheets, the stratigraphic features and their continuity are preserved. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal 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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• W2014605364 title "Late Paleozoic conodonts from ribbon chert delineate imbricate thrusts within the Antler Formation of the Slide Mountain terrane, central British Columbia" @default.
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