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• W2258481618 abstract "Research Article| June 01, 2015 Architecture and Evolution of A Regressive, Tide-Influenced Marginal Marine Succession, Drumheller, Alberta, Canada R.B. Ainsworth; R.B. Ainsworth 1Australian School of Petroleum, University of Adelaide, Adelaide SA 5005, Australia *Present Address: Chevron Global Technology Centre, 250 St Georges Terrace, Perth WA 6000, Australia e-mail: bruce.ainsworth@chevron.com Search for other works by this author on: GSW Google Scholar B.K. Vakarelov; B.K. Vakarelov 1Australian School of Petroleum, University of Adelaide, Adelaide SA 5005, Australia Search for other works by this author on: GSW Google Scholar C. Lee; C. Lee 1Australian School of Petroleum, University of Adelaide, Adelaide SA 5005, Australia Search for other works by this author on: GSW Google Scholar J.A MacEachern; J.A MacEachern 2ARISE, Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia, Canada Search for other works by this author on: GSW Google Scholar A.E. Montgomery; A.E. Montgomery 2ARISE, Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia, Canada Search for other works by this author on: GSW Google Scholar L.P. Ricci; L.P. Ricci 2ARISE, Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia, Canada Search for other works by this author on: GSW Google Scholar S.E. Dashtgard S.E. Dashtgard 2ARISE, Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia, Canada Search for other works by this author on: GSW Google Scholar Author and Article Information R.B. Ainsworth *Present Address: Chevron Global Technology Centre, 250 St Georges Terrace, Perth WA 6000, Australia 1Australian School of Petroleum, University of Adelaide, Adelaide SA 5005, Australia B.K. Vakarelov 1Australian School of Petroleum, University of Adelaide, Adelaide SA 5005, Australia C. Lee 1Australian School of Petroleum, University of Adelaide, Adelaide SA 5005, Australia J.A MacEachern 2ARISE, Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia, Canada A.E. Montgomery 2ARISE, Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia, Canada L.P. Ricci 2ARISE, Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia, Canada S.E. Dashtgard 2ARISE, Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia, Canada e-mail: bruce.ainsworth@chevron.com Publisher: SEPM Society for Sedimentary Geology Received: 15 Jun 2014 Accepted: 14 Feb 2015 First Online: 09 Mar 2017 Online ISSN: 1938-3681 Print ISSN: 1527-1404 Copyright © 2015, SEPM (Society for Sedimentary Geology) Journal of Sedimentary Research (2015) 85 (6): 596–625. https://doi.org/10.2110/jsr.2015.33 Article history Received: 15 Jun 2014 Accepted: 14 Feb 2015 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation R.B. Ainsworth, B.K. Vakarelov, C. Lee, J.A MacEachern, A.E. Montgomery, L.P. Ricci, S.E. Dashtgard; Architecture and Evolution of A Regressive, Tide-Influenced Marginal Marine Succession, Drumheller, Alberta, Canada. Journal of Sedimentary Research 2015;; 85 (6): 596–625. doi: https://doi.org/10.2110/jsr.2015.33 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 SocietyJournal of Sedimentary Research Search Advanced Search Abstract: Tide-dominated and tide-influenced clastic depositional environments are typically interpreted to be associated with landward-stepping or transgressive systems. Here, we present an example of an overall regressive succession dominated by high-frequency sequences that exhibit abundant sedimentary and ichnological evidence of tidal processes. These strata comprise the Campanian Bearpaw–Horseshoe Canyon Formation transition exposed near Drumheller, Alberta, Canada. The clastic marine to marginal-marine sediments were deposited in mixed-process (wave-, tide-, and fluvial-influenced) depositional environments along the western margin of a foreland basin. The deposits are subdivided into six relatively thin (10 m on average), high-frequency (∼ 140,000 years), transgressive–regressive (T-R) sequences (A to F).Outcrop sedimentary logs and hand-held gamma-ray profiles were correlated to subsurface data (4 cored wells and 75 wells with wireline logs) within an area of 22 km × 16 km in order to generate a 3D geocellular computer model. This model along with paleocurrent data from outcrop were used to analyze the stratigraphic architecture and evolution of the succession.The evolution of the successive T-R sequences was mapped on a subregional scale using the 3D geocellular model. The orientations of the paleoshorelines rotate in a predictable manner during transgression and regression. Transgressive shorelines are oriented approximately S–N and rotate clockwise during regression to approximately SW–NE. The rotations are attributed to the paleogeography of the region, with the study area interpreted to sit on the western flank of a large structurally controlled embayment.The progradational high-frequency sequence set is dominated by tide-influenced strata and clearly demonstrates that tidal deposits can be preserved in both regressive as well as transgressive successions. Tidal influence in this regressive setting is attributed to shallow water depths on a wide shelf, which resulted in amplification of the tidal wave as it moved across the shelf. The embayed character of the coastline may also have augmented this effect. Tidal range is estimated to have been mesotidal to macrotidal. A modern partial analogue for the Horseshoe Canyon systems is identified from the tropical Mitchell River Delta in the Gulf of Carpentaria, Queensland, Australia. This delta system is analogous in terms of its tide-influenced facies, mesotidal range, low-gradient shelf with accompanying shallow water depths, the mixed-process character of its shoreline systems, and its horizontal to falling shoreline trajectory. 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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• W2258481618 date "2015-06-11" @default.
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• W2258481618 title "Architecture and Evolution of A Regressive, Tide-Influenced Marginal Marine Succession, Drumheller, Alberta, Canada" @default.
• W2258481618 cites W1558464430 @default.
• W2258481618 cites W1588480515 @default.
• W2258481618 cites W1751425781 @default.
• W2258481618 cites W1853509959 @default.
• W2258481618 cites W1965846255 @default.
• W2258481618 cites W1969557417 @default.
• W2258481618 cites W1970725183 @default.
• W2258481618 cites W1973860858 @default.
• W2258481618 cites W1974560934 @default.
• W2258481618 cites W1976047573 @default.
• W2258481618 cites W1980139141 @default.
• W2258481618 cites W1980520124 @default.
• W2258481618 cites W1981440187 @default.
• W2258481618 cites W1984802995 @default.
• W2258481618 cites W1990269982 @default.
• W2258481618 cites W1993686377 @default.
• W2258481618 cites W2002200719 @default.
• W2258481618 cites W2007748098 @default.
• W2258481618 cites W2010610706 @default.
• W2258481618 cites W2017043635 @default.
• W2258481618 cites W2017486262 @default.
• W2258481618 cites W2021041237 @default.
• W2258481618 cites W2023036480 @default.
• W2258481618 cites W2037350614 @default.
• W2258481618 cites W2043869293 @default.
• W2258481618 cites W2049644657 @default.
• W2258481618 cites W2065034360 @default.
• W2258481618 cites W2067353349 @default.
• W2258481618 cites W2069598620 @default.
• W2258481618 cites W2077196926 @default.
• W2258481618 cites W2080830021 @default.
• W2258481618 cites W2083947006 @default.
• W2258481618 cites W2086727967 @default.
• W2258481618 cites W2094581504 @default.
• W2258481618 cites W2094765754 @default.
• W2258481618 cites W2098757316 @default.
• W2258481618 cites W2106670600 @default.
• W2258481618 cites W2107694080 @default.
• W2258481618 cites W2111364173 @default.
• W2258481618 cites W2117103196 @default.
• W2258481618 cites W2124565668 @default.
• W2258481618 cites W2125279311 @default.
• W2258481618 cites W2129531365 @default.
• W2258481618 cites W2130299803 @default.
• W2258481618 cites W2131513523 @default.
• W2258481618 cites W2141340156 @default.
• W2258481618 cites W2144414810 @default.
• W2258481618 cites W2156678727 @default.
• W2258481618 cites W2160804234 @default.
• W2258481618 cites W2171679435 @default.
• W2258481618 cites W2173216887 @default.
• W2258481618 cites W2242032389 @default.
• W2258481618 cites W2252313559 @default.
• W2258481618 cites W2263190699 @default.
• W2258481618 cites W2291952232 @default.
• W2258481618 cites W2307588388 @default.
• W2258481618 cites W2397433527 @default.
• W2258481618 cites W2414757987 @default.
• W2258481618 cites W2466078123 @default.
• W2258481618 cites W2908799244 @default.
• W2258481618 cites W2911188857 @default.
• W2258481618 cites W3112941943 @default.
• W2258481618 cites W647463333 @default.
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• W2258481618 doi "https://doi.org/10.2110/jsr.2015.33" @default.
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