Mapping the Belly River Group in Alberta

Total Page:16

File Type:pdf, Size:1020Kb

Mapping the Belly River Group in Alberta Mapping the Belly River Group in Alberta Paul Glombick, Ben Hathway, Shilong Mei, Christopher Banks, and Duncan Hay As part of an initiative to create a digital atlas of the near-surface geology of Alberta, the Alberta Geological Survey is undertaking a regional study of the Belly River Group in central and southern Alberta. The goal of the study is to delineate regional stratigraphic surfaces within the Belly River Group, particularly within 500 metres of the surface. The primary method of investigation is a series of closely-spaced subsurface cross-sections, with targeted field work on key stratigraphic intervals. The Belly River Group represents a westward-thickening, third-order clastic sequence deposited within the Western Canadian Foreland Basin during the Campanian. In southern and south- central Alberta, the Belly River Group has been divided into the Foremost, Oldman, and Dinosaur Park formations. The Dinosaur Park Formation thins from west to east and is separated from the underlying Oldman Formation by a regional discontinuity that can be mapped over much of central and southern Alberta (Eberth and Hamblin, 1993; Hamblin, 1997a). The Oldman Formation can be subdivided into an upper, fine-grained “silt unit” and a lower sandstone unit (Hamblin, 1997b). The sandstone unit overlies the Taber coal zone, which situated at the top of the Foremost Formation, where present. In eastern Alberta, there is a complex interfingering between nonmarine and marginal marine rocks of the lower Belly River Group and fine-grained marine rocks of the Lea Park Formation. References Eberth, D.A. and Hamblin, A.P. 1993. Tectonic, stratigraphic, and sedimentologic significance of a regional discontinuity in the upper Judith River Formation (Belly River wedge) of southern Alberta, Saskatchewan, and northern Montana. Canadian Journal of Earth Sciences, v. 30, p. 174-200. Hamblin, A.P. 1997a. Regional distribution and dispersal of the Dinosaur Park Formation, Belly River Group, surface and subsurface of southern Alberta. Bulletin of Canadian Petroleum Geology, v. 45, p. 377–399. Hamblin, A.P. 1997b. Stratigraphic architecture of the Oldman Formation, Belly River Group, surface and subsurface of southern Alberta. Bulletin of Canadian Petroleum Geology, v. 45, p. 155-177. GeoCanada 2010 – Working with the Earth 1 .
Recommended publications
  • Soil Survey and Reclamation Suitability Evaluation of the Proposed Nova Gas Transmission Ltd
    NOVA Gas Transmission Ltd. Environmental and Socio-Economic Assessment Norma Transmission Pipeline Project February 2013/8660 APPENDIX 3 SOIL SURVEY AND RECLAMATION SUITABILITY EVALUATION OF THE PROPOSED NOVA GAS TRANSMISSION LTD. NORMA TRANSMISSION PIPELINE PROJECT Page A3-1 SOIL SURVEY AND RECLAMATION SUITABILITY EVALUATION of the PROPOSED NOVA GAS TRANSMISSION LTD. NORMA TRANSMISSION PIPELINE Prepared for: TERA ENVIRONMENTAL CONSULTANTS On behalf of: NOVA GAS TRANSMISSION LTD. Prepared by: MENTIGA PEDOLOGY CONSULTANTS LTD. A.G. Twardy, M.Sc., P.Ag. B. Chernipeski, B.Sc., P.Ag. February 2013 11037B.1 TABLE OF CONTENTS 1.0 INTRODUCTION ............................................................................................................. 1 2.0 THE STUDY AREA .......................................................................................................... 3 2.1 Location and Extent ............................................................................................ 3 2.2 Bedrock Geology ................................................................................................ 3 2.3 Surficial Materials and Landform ........................................................................ 3 2.4 General Soil Patterns .......................................................................................... 4 2.5 Present Land Use ............................................................................................... 4 3.0 SOILS ...................................................................................................................
    [Show full text]
  • Post-Carboniferous Stratigraphy, Northeastern Alaska by R
    Post-Carboniferous Stratigraphy, Northeastern Alaska By R. L. DETTERMAN, H. N. REISER, W. P. BROSGE,and]. T. DUTRO,JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 886 Sedirnentary rocks of Permian to Quaternary age are named, described, and correlated with standard stratigraphic sequences UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1975 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Detterman, Robert L. Post-Carboniferous stratigraphy, northeastern Alaska. (Geological Survey Professional Paper 886) Bibliography: p. 45-46. Supt. of Docs. No.: I 19.16:886 1. Geology-Alaska. I. Detterman, Robert L. II. Series: United States. Geological Survey. Professional Paper 886. QE84.N74P67 551.7'6'09798 74-28084 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02687-2 CONTENTS Page Page Abstract __ _ _ _ _ __ __ _ _ _ _ _ _ _ _ _ _ _ _ __ __ _ _ _ _ _ _ __ __ _ _ __ __ __ _ _ _ _ __ 1 Stratigraphy__:_Continued Introduction __________ ----------____ ----------------____ __ 1 Kingak Shale ---------------------------------------- 18 Purpose and scope ----------------------~------------- 1 Ignek Formation (abandoned) -------------------------- 20 Geographic setting ------------------------------------ 1 Okpikruak Formation (geographically restricted) ________ 21 Previous work and acknowledgments ------------------ 1 Kongakut Formation ----------------------------------
    [Show full text]
  • The Dinosaur Park - Bearpaw Formation Transition in the Cypress Hills Region of Southwestern Saskatchewan, Canada Meagan M
    The Dinosaur Park - Bearpaw Formation Transition in the Cypress Hills Region of Southwestern Saskatchewan, Canada Meagan M. Gilbert Department of Geological Sciences, University of Saskatchewan; [email protected] Summary The Upper Cretaceous Dinosaur Park Formation (DPF) is a south- and eastward-thinning fluvial to marginal marine clastic-wedge in the Western Canadian Sedimentary Basin. The DPF is overlain by the Bearpaw Formation (BF), a fully marine clastic succession representing the final major transgression of the epicontinental Western Interior Seaway (WIS) across western North America. In southwestern Saskatchewan, the DPF is comprised of marginal marine coal, carbonaceous shale, and heterolithic siltstone and sandstone grading vertically into marine sandstone and shale of the Bearpaw Formation. Due to Saskatchewan’s proximity to the paleocoastline, 5th order transgressive cycles resulted in the deposition of multiple coal seams (Lethbridge Coal Zone; LCZ) in the upper two-thirds of the DPF in the study area. The estimated total volume of coal is 48109 m3, with a gas potential of 46109 m3 (Frank, 2005). The focus of this study is to characterize the facies and facies associations of the DPF, the newly erected Manâtakâw Member, and the lower BF in the Cypress Hills region of southwestern Saskatchewan utilizing core, outcrop, and geophysical well log data. This study provides a comprehensive sequence stratigraphic overview of the DPF-BF transition in Saskatchewan and the potential for coalbed methane exploration. Introduction The Dinosaur Park and Bearpaw Formations in Alberta, and its equivalents in Montana, have been the focus of several sedimentologic and stratigraphic studies due to exceptional outcrop exposure and extensive subsurface data (e.g., McLean, 1971; Wood, 1985, 1989; Eberth and Hamblin, 1993; Tsujita, 1995; Catuneanu et al., 1997; Hamblin, 1997; Rogers et al., 2016).
    [Show full text]
  • Histology and Ontogeny of Pachyrhinosaurus Nasal Bosses By
    Histology and Ontogeny of Pachyrhinosaurus Nasal Bosses by Elizabeth Kruk A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Systematics and Evolution Department of Biological Sciences University of Alberta © Elizabeth Kruk, 2015 Abstract Pachyrhinosaurus is a peculiar ceratopsian known only from Upper Cretaceous strata of Alberta and the North Slope of Alaska. The genus consists of three described species Pachyrhinosaurus canadensis, Pachyrhinosaurus lakustai, and Pachyrhinosaurus perotorum that are distinguishable by cranial characteristics, including parietal horn shape and orientation, absence/presence of a rostral comb, median parietal bar horns, and profile of the nasal boss. A fourth species of Pachyrhinosaurus is described herein and placed into its phylogenetic context within Centrosaurinae. This new species forms a polytomy at the crown with Pachyrhinosaurus canadensis and Pachyrhinosaurus perotorum, with Pachyrhinosaurus lakustai falling basal to that polytomy. The diagnostic features of this new species are an apomorphic, laterally curved Process 3 horns and a thick longitudinal ridge separating the supraorbital bosses. Another focus is investigating the ontogeny of Pachyrhinosaurus nasal bosses in a histological context. Previously, little work has been done on cranial histology in ceratopsians, focusing instead on potential integumentary structures, the parietals of Triceratops, and how surface texture relates to underlying histological structures. An ontogenetic series is established for the nasal bosses of Pachyrhinosaurus at both relative (subadult versus adult) and fine scale (Stages 1-5). It was demonstrated that histology alone can indicate relative ontogenetic level, but not stages of a finer scale. Through Pachyrhinosaurus ontogeny the nasal boss undergoes increased vascularity and secondary remodeling with a reduction in osteocyte lacunar density.
    [Show full text]
  • Dinosaur Eggshells from the Lower Maastrichtian St. Mary River Formation of Southern Alberta, Canada
    Canadian Journal of Earth Sciences Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern Alberta, Canada Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2017-0195.R1 Manuscript Type: Article Date Submitted by the Author: 13-Nov-2017 Complete List of Authors: Voris, Jared; University of Calgary, Geoscience; Zelenitsky, Darla; Department of Geoscience, Tanaka, Kohei; Nagoya Daigaku Hakubutsukan; University of Calgary, DepartmentDraft of Geoscience Therrien, François; Royal Tyrrell Museum of Palaeontology, Is the invited manuscript for consideration in a Special N/A Issue? : Keyword: eggshell, dinosaur, Cretaceous, Maastrichtian, Alberta https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 47 Canadian Journal of Earth Sciences 1 2 3 4 5 6 7 8 9 Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern 10 Alberta, Canada 11 12 Jared T. Voris, Darla K. Zelenitsky,Draft François Therrien, Kohei Tanaka 13 J. T. Voris, D. K. Zelenitsky, and K. Tanaka. Department of Geoscience, University of 14 Calgary, 2500 University Dr. NW, Calgary, AB T2N 1N4, Canada; [email protected], 15 [email protected], [email protected] 16 K. Tanaka. Nagoya University Museum, Nagoya University Furocho, Chikusa-Ku, Nagoya, 17 464-8601, Japan; [email protected] 18 F. Therrien. Royal Tyrrell Museum of Palaeontology, Box 7500, Drumheller, AB T0J 0Y0, 19 Canada.; [email protected] 20 1 https://mc06.manuscriptcentral.com/cjes-pubs Canadian Journal of Earth Sciences Page 2 of 47 1 2 Abstract–North America is known for its rich uppermost Cretaceous record of dinosaur egg 3 remains, although a notable fossil gap exists during the lower Maastrichtian.
    [Show full text]
  • Belly River Group), Suffield Area, South Saskatchewan River Valley, Southeastern Alberta (NTS 72L/03) ERCB/AGS Open File Report 2011-06
    ERCB/AGS Open File Report 2011-06 Measured Outcrop Section T13-R9W4-01 of the Foremost and Oldman Formations (Belly River Group), Suffield Area, South Saskatchewan River Valley, Southeastern Alberta (NTS 72L/03) ERCB/AGS Open File Report 2011-06 Measured Outcrop Section T13-R9W4-01 of the Foremost and Oldman Formations (Belly River Group), Suffield Area, South Saskatchewan River Valley, Southeastern Alberta (NTS 72L/03) B. Hathway, C.J. Banks, D.C. Hay and S. Mei Energy Resources Conservation Board Alberta Geological Survey July 2011 ©Her Majesty the Queen in Right of Alberta, 2011 ISBN 978-0-7785-8647-0 The Energy Resources Conservation Board/Alberta Geological Survey (ERCB/AGS), its employees and contractors make no warranty, guarantee or representation, express or implied, or assume any legal liability regarding the correctness, accuracy, completeness or reliability of this publication. Any reference to proprietary software and/or any use of proprietary data formats do not constitute endorsement by ERCB/AGS of any manufacturer's product. If you use information from this publication in other publications or presentations, please acknowledge the ERCB/AGS. We recommend the following reference format: Hathway, B., Banks, C.J., Hay, D.C. and Mei, S. (2011): Measured outcrop section T13-R9W4-01 of the Foremost and Oldman formations (Belly River Group), Suffield area, South Saskatchewan River valley, southeastern Alberta (NTS 72L/03); Energy Resources Conservation Board, ERCB/AGS Open File 2011-06, 14 p. Published July 2011 by: Energy Resources
    [Show full text]
  • Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area
    ERCB/AGS Special Report 093 Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area Stefan Bachu Maja Buschkuehle Kristine Haug Karsten Michael Alberta Geological Survey Alberta Energy and Utilities Board ©Her Majesty the Queen in Right of Alberta, 2008 ISBN 978-0-7785-6950-3 The Energy Resources Conservation Board/Alberta Geological Survey (ERCB/AGS) and its employees and contractors make no warranty, guarantee or representation, express or implied, or assume any legal liability regarding the correctness, accuracy, completeness or reliability of this publication. Any digital data and software supplied with this publication are subject to the licence conditions. The data are supplied on the understanding that they are for the sole use of the licensee, and will not be redistributed in any form, in whole or in part, to third parties. Any references to proprietary software in the documentation, and/or any use of proprietary data formats in this release, do not constitute endorsement by the ERCB/AGS of any manufacturer's product. If this product is an ERCB/AGS Special Report, the information is provided as received from the author and has not been edited for conformity to ERCB/AGS standards. When using information from this publication in other publications or presentations, due acknowledgment should be given to the ERCB/AGS. The following reference format is recommended: Bachu, S., Buschkuehle, M., Haug, K., Michael, K. (2008): Subsurface characterization of the Pembina-Wabamun acid-gas injection area; Energy Resources Conservation Board, ERCB/AGS Special Report 093, 60 p.
    [Show full text]
  • A New Maastrichtian Species of the Centrosaurine Ceratopsid Pachyrhinosaurus from the North Slope of Alaska
    A new Maastrichtian species of the centrosaurine ceratopsid Pachyrhinosaurus from the North Slope of Alaska ANTHONY R. FIORILLO and RONALD S. TYKOSKI Fiorillo, A.R. and Tykoski, R.S. 2012. A new Maastrichtian species of the centrosaurine ceratopsid Pachyrhinosaurus from the North Slope of Alaska. Acta Palaeontologica Polonica 57 (3): 561–573. The Cretaceous rocks of the Prince Creek Formation contain the richest record of polar dinosaurs found anywhere in the world. Here we describe a new species of horned dinosaur, Pachyrhinosaurus perotorum that exhibits an apomorphic character in the frill, as well as a unique combination of other characters. Phylogenetic analysis of 16 taxa of ceratopsians failed to resolve relationships between P. perotorum and other Pachyrhinosaurus species (P. canadensis and P. lakustai). P. perotorum shares characters with each of the previously known species that are not present in the other, including very large nasal and supraorbital bosses that are nearly in contact and separated only by a narrow groove as in P. canadensis, and a rostral comb formed by the nasals and premaxillae as in P. lakustai. P. perotorum is the youngest centrosaurine known (70–69 Ma), and the locality that produced the taxon, the Kikak−Tegoseak Quarry, is close to the highest latitude for recovery of ceratopsid remains. Key words: Dinosauria, Centrosaurinae, Cretaceous, Prince Creek Formation, Kikak−Tegoseak Quarry, Arctic. Anthony R. Fiorillo [[email protected]] and Ronald S. Tykoski [[email protected]], Perot Museum of Nature and Science, 2201 N. Field Street, Dallas, TX 75202, USA. Received 4 April 2011, accepted 23 July 2011, available online 26 August 2011.
    [Show full text]
  • Competition Structured a Late Cretaceous Megaherbivorous Dinosaur Assemblage Jordan C
    www.nature.com/scientificreports OPEN Competition structured a Late Cretaceous megaherbivorous dinosaur assemblage Jordan C. Mallon 1,2 Modern megaherbivore community richness is limited by bottom-up controls, such as resource limitation and resultant dietary competition. However, the extent to which these same controls impacted the richness of fossil megaherbivore communities is poorly understood. The present study investigates the matter with reference to the megaherbivorous dinosaur assemblage from the middle to upper Campanian Dinosaur Park Formation of Alberta, Canada. Using a meta-analysis of 21 ecomorphological variables measured across 14 genera, contemporaneous taxa are demonstrably well-separated in ecomorphospace at the family/subfamily level. Moreover, this pattern is persistent through the approximately 1.5 Myr timespan of the formation, despite continual species turnover, indicative of underlying structural principles imposed by long-term ecological competition. After considering the implications of ecomorphology for megaherbivorous dinosaur diet, it is concluded that competition structured comparable megaherbivorous dinosaur communities throughout the Late Cretaceous of western North America. Te question of which mechanisms regulate species coexistence is fundamental to understanding the evolution of biodiversity1. Te standing diversity (richness) of extant megaherbivore (herbivores weighing ≥1,000 kg) com- munities appears to be mainly regulated by bottom-up controls2–4 as these animals are virtually invulnerable to top-down down processes (e.g., predation) when fully grown. Tus, while the young may occasionally succumb to predation, fully-grown African elephants (Loxodonta africana), rhinoceroses (Ceratotherium simum and Diceros bicornis), hippopotamuses (Hippopotamus amphibius), and girafes (Girafa camelopardalis) are rarely targeted by predators, and ofen show indiference to their presence in the wild5.
    [Show full text]
  • Resolution Revolution: Advances in Palynostratigraphy Over Three Decades Dennis R
    Resolution Revolution: Advances in Palynostratigraphy Over Three Decades Dennis R. Braman, Royal Tyrrell Museum of Palaeontology, Box 7500, Drumheller, Alberta, T0J 0Y0, [email protected] Significant improvements in the ability of palynology to solve stratigraphic problems in the Upper Cretaceous-Paleocene strata of the southern part of the Alberta Basin have been made over the last three decades. This progress has developed in conjunction with similar improvements in other correlation tools including radiometric dating, strontium isotope dating, magnetostratigraphy, lithostratigraphy, and ammonite biostratigraphy. It is the purpose of this presentation to select a few representative examples which illustrate some of these advances with emphasis on the palynostratigraphy. Much of the material used in this research comes from surface exposures with the oldest significant exposures on the plains area being those of the Milk River Formation. Based on comparisons of the paleomagnetostratigraphic results of Leahy and Lerbekmo (1995) compared to those of Europe, Braman (2002) concluded that nearly the entire formation was Santonian in age in Alberta and there was a significant time gap of 2 to 3 million years between the Milk River and overlying Pakowki Formation in southern Alberta. A portion of this missing time interval is accounted for in the upper unnamed member of the Eagle Formation in the vicinity of the Missouri River in Montana between Eagle Creek and the Bearpaw Mountains (Payenberg et al., 2002). This member is entirely marine and represents a transgressive event that is entirely missing from exposures in southern plains area of Alberta. The Telegraph Creek, Virgelle, and Deadhorse Coulee members of the Milk River Formation can be directly correlated with the Telegraph Creek Formation and Virgelle and unnamed middle members of the Eagle Formation in that they have similar palynomorph assemblages.
    [Show full text]
  • THE BIBLIOGRAPHY of HADROSAURIAN DINOSAURS the First 150 Years: 1856 - 2006
    THE BIBLIOGRAPHY OF HADROSAURIAN DINOSAURS The First 150 Years: 1856 - 2006. complied by M.K. Brett-Surman © Smithsonian Institution 1985-2008 The Department of Paleobiology of the National Museum of Natural History, Smithsonian Institution, currently houses approximately 44 million fossil plant, invertebrate, and vertebrate fossils in more than 480 separate collections. In addition, Paleobiology also maintains a reference collection of over 120,000 stratigraphic and sediment samples. This listing represents a service provided to the public as part of our Outreach Program and as part of the Smithsonian Institution’s mission "for the increase and diffusion of knowledge...". Papers are listed by author and year. Author's names are capitalized. The viewer should be aware of any searches that are case sensitive. The papers listed here, in a majority of instances, do NOT contain abstracts, papers on ichnites, or popular articles or books, unless they present new information or cover an aspect of the history of dinosaur paleontology. At present, some of the legacy software that was used to maintain this list only allowed basic ASCII characters, therefore foreign accents (such as in French and Spanish) did not translate. This will be fixed at a later date. The Bibliography of Hadrosaurian Dinosaurs was written, compiled, and maintained by M.K. Brett-Surman, (Museum Specialist), P.O. Box 37012, Department of Paleobiology, National Museum of Natural History, MRC-121, Washington, DC 20013-7012. He can be reached electronically at: [email protected]., and by FAX at 202-786-2832. Please send all corrections and additions to the e-mail address. This file will be no longer be updated, except for entries prior to 2007.
    [Show full text]
  • Bedrock Geology of Alberta
    Alberta Geological Survey Map 600 Legend Bedrock Geology of Alberta Southwestern Plains Southeastern Plains Central Plains Northwestern Plains Northeastern Plains NEOGENE (± PALEOGENE) NEOGENE ND DEL BONITA GRAVELS: pebble gravel with some cobbles; minor thin beds and lenses NH HAND HILLS FORMATION: gravel and sand, locally cemented into conglomerate; gravel of sand; pebbles consist primarily of quartzite and argillite with minor amounts of sandstone, composed of mainly quartzite and sandstone with minor amounts of chert, arkose, and coal; fluvial amygdaloidal basalt, and diabase; age poorly constrained; fluvial PALEOGENE PALEOGENE PALEOGENE (± NEOGENE) PALEOGENE (± NEOGENE) UPLAND GRAVEL: gravel composed of mainly white quartzite cobbles and pebbles with lesser amounts of UPLAND GRAVEL: gravel capping the Clear Hills, Halverson Ridge, and Caribou Mountains; predominantly .C CYPRESS HILLS FORMATION: gravel and sand, locally cemented to conglomerate; mainly quartzite .G .G and sandstone clasts with minor chert and quartz component; fluvial black chert pebbles; sand matrix; minor thin beds and lenses of sand; includes gravel in the Swan Hills area; white quartzite cobbles and pebbles with lesser amounts of black chert pebbles; quartzite boulders occur in the age poorly constrained; fluvial Clear Hills and Halverson Ridge gravels; sand matrix; ages poorly constrained; extents poorly defined; fluvial .PH PORCUPINE HILLS FORMATION: olive-brown mudstone interbedded with fine- to coarse-grained, .R RAVENSCRAG FORMATION: grey to buff mudstone
    [Show full text]