AER/AGS Open File Report: Mapping Formation-Top Offsets in The

Total Page:16

File Type:pdf, Size:1020Kb

AER/AGS Open File Report: Mapping Formation-Top Offsets in The AER/AGS Open File Report 2020-02 Mapping Formation-Top Offsets in the Southwestern Alberta Plains, Canada: Methodology and Results AER/AGS Open File Report 2020-02 Mapping Formation-Top Offsets in the Southwestern Alberta Plains, Canada: Methodology and Results S. Mei and R. Schultz Alberta Energy Regulator Alberta Geological Survey October 2020 ©Her Majesty the Queen in Right of Alberta, 2020 ISBN 978-1-4601-4606-07 The Alberta Energy Regulator / Alberta Geological Survey (AER/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 references to proprietary software and/or any use of proprietary data formats do not constitute endorsement by the AER/AGS of any manufacturer’s product. If you use information from this publication in other publications or presentations, please acknowledge the AER/AGS. We recommend the following reference format: Mei, S and R. Schultz (2020): Mapping formation-top offsets in the southwestern Alberta Plains, Canada: methodology and results; Alberta Energy Regulator / Alberta Geological Survey, AER/AGS Open File Report 2020-02, 34 p. Publications in this series have undergone only limited review and are released essentially as submitted by the author. Published October 2020 by: Alberta Energy Regulator Alberta Geological Survey 4th Floor, Twin Atria Building 4999 – 98th Avenue Edmonton, AB T6B 2X3 Canada Tel: 780.638.4491 Fax: 780.422.1459 Email: [email protected] Website: www.ags.aer.ca AER/AGS Open File Report 2020-02 • iii Contents Acknowledgements ....................................................................................................................................... v Abstract ........................................................................................................................................................ vi 1 Introduction.............................................................................................................................................. 7 2 Geological Background ........................................................................................................................... 9 3 Data and Sources of Error ...................................................................................................................... 15 4 Methodology .......................................................................................................................................... 16 4.1 Data Cleaning and Refinement ...................................................................................................... 16 4.2 Mapping Structural Features .......................................................................................................... 17 4.3 Initial Characterization of Offsets .................................................................................................. 18 4.4 Comparison with Conventional Methods ...................................................................................... 18 5 Results and Interpretation ...................................................................................................................... 19 5.1 Comparison to Previously Reported Faults ................................................................................... 27 6 Conclusions............................................................................................................................................ 30 7 References.............................................................................................................................................. 31 Tables Table 1. Offsets of faults F1–F5 as shown in Figure 13. ............................................................................ 30 Figures Figure 1. Location of the study area in southwestern Alberta. ..................................................................... 8 Figure 2. Stratigraphic nomenclature for the study area. .............................................................................. 9 Figure 3. Bedrock geology map of the study area. ..................................................................................... 11 Figure 4. Generalized geological cross-section of the study area. .............................................................. 12 Figure 5. Previously reported structures in the study area. ......................................................................... 14 Figure 6. The trend surface modelled for the lower Bearpaw Formation flooding surface, clipped to the erosional edge to the east, and the data limit and deformation front to the west. .................................. 20 Figure 7. Residual map of the lower Bearpaw Formation flooding surface, clipped to the erosional edge to the east: (a) includes control wells and (b) map of (a) with interpreted offsets. .................................... 21 Figure 8. Residual map of the Milk River Formation top in the study area: (a) includes control wells and (b) map of (a) with interpreted offsets. .................................................................................................. 22 Figure 9. Residual map of the base of the Fish Scales Formation (BFS) in the study area: (a) includes control wells and (b) map of (a) with interpreted offsets....................................................................... 23 Figure 10. Structure cross-section showing the horizons and log characteristics of the lower Bearpaw Formation surface, the Milk River top and the base of the Fish Scales Formation, as well as the offsets of faults F1 to F4 and possibly the southern extension of fault F5 of Lemieux (1999). ........................ 25 Figure 11. Isopach map of the interval from the base of the Fish Scales Formation (BFS) to the Milk River Formation top: (a) includes control wells and (b) map of (a) with interpreted lineaments. ......... 26 Figure 12. Interpreted offsets from the lower Bearpaw Formation flooding surface, Milk River Formation top, and base of the Fish Scales Formation (BFS) overlain on the isopach map of the interval from the BFS to the top of Milk River Formation. ............................................................................................... 27 Figure 13. Comparison of mapped subsurface linear offsets with previously reported faults. ................... 28 AER/AGS Open File Report 2020-02 • iv Acknowledgements We wish to thank D.I. Pană, D. Palombi, K.E. MacCormack, T.E. Hauck, M. Grobe, and K. Haug, whose editorial review and technical commentaries considerably improved the manuscript. AER/AGS Open File Report 2020-02 • v Abstract This report presents the results of subsurface bedrock structure mapping in southwestern Alberta, Canada, using a methodology that assesses formation-top offsets. Three stratigraphic horizons were selected for mapping subsurface bedrock offsets: the base of the Fish Scales Formation, the top of the Milk River Formation, and the lower Bearpaw Formation flooding surface. The selected surfaces represent, or are close to, marine flooding surfaces in this area and can be considered to approximate a flat-lying surface (datum) and, therefore, are ideal for mapping post-depositional structures. A bedrock offset is defined in this report as any lineament or possible vertical displacement of a bedrock horizon that has been detected using geostatistical analysis of well-log data. This methodology identified numerous potential offsets which have been highlighted using residual maps of these three surfaces. The offset features identified from these surfaces were compared to each other, and to an isopach map of the interval from the base of the Fish Scales Formation to the top of Milk River Formation to evaluate whether these offsets represent potential growth faults. Some of the offsets mapped in this report were found to coincide with previously reported faults, which were identified at isolated riverbank outcrops and interpreted from seismic reflection surveys, and allow for determination of fault orientation and extent. The other offsets highlighted in this report may represent potential faults or differential compaction and highlight areas of geological interest for future structural analysis. AER/AGS Open File Report 2020-02 • vi 1 Introduction In recent years, the Exshaw Formation and adjacent units, the underlying carbonates of the Big Valley and upper Stettler formations and the overlying basal Banff Formation, have emerged as unconventional tight oil resource plays in southwestern Alberta with the advent of hydraulic fracturing (fracking) techniques in horizontal wells. As a result, this area has experienced increased oil and gas development activities and capital investment since 2009 (Zaitlin et al., 2011). The AGS seismicity monitoring network detected a cluster of earthquakes in southwestern Alberta, which may be related to fault reactivation potentially induced by hydraulic fracturing (Schultz et al., 2015). Further investigation into this cluster of earthquakes requires detailed study of the bedrock structure, which may have significant impact on induced seismic events in this area. This study attempts to map subsurface formation-top offsets in southwestern Alberta using well-log data and geostatistical analysis. We define an offset as any lineament of relatively abrupt elevation change of a formation top or bedrock horizon that can be detected using the methodology proposed by Mei
Recommended publications
  • Theropod Teeth from the Upper Maastrichtian Hell Creek Formation “Sue” Quarry: New Morphotypes and Faunal Comparisons
    Theropod teeth from the upper Maastrichtian Hell Creek Formation “Sue” Quarry: New morphotypes and faunal comparisons TERRY A. GATES, LINDSAY E. ZANNO, and PETER J. MAKOVICKY Gates, T.A., Zanno, L.E., and Makovicky, P.J. 2015. Theropod teeth from the upper Maastrichtian Hell Creek Formation “Sue” Quarry: New morphotypes and faunal comparisons. Acta Palaeontologica Polonica 60 (1): 131–139. Isolated teeth from vertebrate microfossil localities often provide unique information on the biodiversity of ancient ecosystems that might otherwise remain unrecognized. Microfossil sampling is a particularly valuable tool for doc- umenting taxa that are poorly represented in macrofossil surveys due to small body size, fragile skeletal structure, or relatively low ecosystem abundance. Because biodiversity patterns in the late Maastrichtian of North American are the primary data for a broad array of studies regarding non-avian dinosaur extinction in the terminal Cretaceous, intensive sampling on multiple scales is critical to understanding the nature of this event. We address theropod biodiversity in the Maastrichtian by examining teeth collected from the Hell Creek Formation locality that yielded FMNH PR 2081 (the Tyrannosaurus rex specimen “Sue”). Eight morphotypes (three previously undocumented) are identified in the sample, representing Tyrannosauridae, Dromaeosauridae, Troodontidae, and Avialae. Noticeably absent are teeth attributed to the morphotypes Richardoestesia and Paronychodon. Morphometric comparison to dromaeosaurid teeth from multiple Hell Creek and Lance formations microsites reveals two unique dromaeosaurid morphotypes bearing finer distal denticles than present on teeth of similar size, and also differences in crown shape in at least one of these. These findings suggest more dromaeosaurid taxa, and a higher Maastrichtian biodiversity, than previously appreciated.
    [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]
  • 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]
  • For the Late Cretaceous of Western North America Robert M
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/54 The Kirtlandian, a new land-vertebrate "age" for the Late Cretaceous of western North America Robert M. Sullivan and Spencer G. Lucas, 2003, pp. 369-377 in: Geology of the Zuni Plateau, Lucas, Spencer G.; Semken, Steven C.; Berglof, William; Ulmer-Scholle, Dana; [eds.], New Mexico Geological Society 54th Annual Fall Field Conference Guidebook, 425 p. This is one of many related papers that were included in the 2003 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks.
    [Show full text]
  • Western Interior Seaway
    () . Paleogeo.graphy of the Late Cretaceous of the Western Interior otMfddle North America+­ j?'oal .Blstribution anct,Sedimen~cumulation By Laura N. Robinson Roberts and Mark A. Kirschbaum U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1561 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1995 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director For sale by U.S. Geological Survey, Information Services Box 25286, Federal Center Denver, CO 80225 Any use of trade, product, or finn names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging-in-Publication Data Roberts, Laura N. Robinson. Paleogeography of the Late Cretaceous of the western interior of middle North America : coal distribution and sediment accumulation I by Laura N. Robinson Roberts and Mark A. Kirschbaum. p. em.- (U.S. Geological Survey professional paper ; 1561) Includes bibliographical references. Supt. of Docs. no.: I 19.16: 1561 1. Paleogeography-Cretaceous. 2. Paleogeography-West (U.S.). 3. Coal­ Geology-West (U.S.). I. Kirschbaum, Mark A. II. Title. III. Series. QE50 1.4.P3R63 1995 553.2'1'0978-dc20 94-39032 CIP CONTENTS Abstract........................................................................................................................... 1" Introduction ................................................................................................................... Western Interior Seaway ... .. ... ... ... .. .. ..
    [Show full text]
  • Bulletin Albertavolume 28 • NUMBER 2 JUNE 2013 ALBERTA PALÆONTOLOGICAL SOCIETY
    Palæontological Society Bulletin AlbertaVOLUME 28 • NUMBER 2 www.albertapaleo.org JUNE 2013 ALBERTA PALÆONTOLOGICAL SOCIETY OFFICERS MEMBERSHIP: Any person with a sincere interest in President Wayne Braunberger (403) 278-5154 palaeontology is eligible to present their application for Vice-President Cory Gross (403) 617-2079 membership in the Society. (Please enclose membership Treasurer Mona Marsovsky (403) 547-0182 dues with your request for application.) Secretary Arnold Ingelson (403) 249-6748 Past-President Dan Quinsey (403) 247-3022 Single membership $20.00 annually Family or Institution $25.00 annually DIRECTORS Editor Howard Allen (403) 274-1858 THE BULLETIN WILL BE PUBLISHED QUARTERLY: Membership Vaclav Marsovsky (403) 547-0182 March, June, September and December. Deadline for sub- Programs Harold Whittaker (403) 286-0349 mitting material for publication is the 15th of the month Field Trips (To volunteer contact the President) prior to publication. COMMITTEES Society Mailing Address: Fossil Collection Howard Allen (403) 274-1858 Alberta Palaeontological Society Library Reg Spratley (403) 263-0556 P.O. Box 35111, Sarcee Postal Outlet Public Outreach Cory Gross (403) 617-2079 Calgary, Alberta, Canada T3E 7C7 Social Dan Quinsey (403) 247-3022 (Web: www.albertapaleo.org) Symposium Vaclav Marsovsky (403) 547-0182 Website Vaclav Marsovsky (403) 547-0182 Material for the Bulletin: The Society was incorporated in 1986, as a non-profit Howard Allen, Editor, APS organization formed to: 7828 Hunterslea Crescent, N.W. Calgary, Alberta, Canada T2K 4M2 a. Promote the science of palaeontology through study (E-mail: [email protected]) and education. b. Make contributions to the science by: NOTICE: Readers are advised that opinions expressed in 1) Discovery 2) Collection 3) Description the articles are those of the author and do not necessarily 4) Education of the general public reflect the viewpoint of the Society.
    [Show full text]
  • Evolution and Diversity of Ornithomimid Dinosaurs in the Upper Cretaceous Belly River Group of Alberta
    Evolution and Diversity of Ornithomimid Dinosaurs in the Upper Cretaceous Belly River Group of Alberta by Bradley McFeeters A thesis submitted to the Faculty of Science in partial fulfillment of the requirements for the degree of Master of Science Department of Earth Sciences Carleton University Ottawa, Ontario May, 2015 © 2015 Bradley McFeeters ABSTRACT Ornithomimids (Dinosauria: Theropoda) from the Campanian (Upper Cretaceous) Belly River Group of Alberta have a fossil record that ranges from isolated elements to nearly complete articulated skeletons. The Belly River Group ornithomimids are among the best-known theropods from these deposits, as well as some of the best-known ornithomimids in the world. However, questions remain concerning the identification of the oldest definitive occurrence of these dinosaurs in Alberta, as well as the taxonomic diversity of the articulated material from the Dinosaur Park Formation. These topics have important implications for reconstructing the palaeobiogeographic and phylogenetic history of Ornithomimidae in Laramidia. The literature on all ornithomimosaurs from the Cretaceous of North America is reviewed, with special attention to their taxonomic history and geological context in the Belly River Group. The species Struthiomimus altus has historically contained most of the articulated ornithomimid material from the Belly River Group, but this is not supported by synapomorphic characters in all cases, and the material referred to S. altus is morphologically heterogeneous. An articulated partial skeleton
    [Show full text]
  • Effects of Groundwater Flow on the Distribution of Biogenic Gas in Parts of the Northern Great Plains of Canada and United States
    Effects of Groundwater Flow on the Distribution of Biogenic Gas in Parts of the Northern Great Plains of Canada and United States Scientific Investigations Report 2010−5251 U.S. Department of the Interior U.S. Geological Survey COVER The Cypress Hills Tertiary remnant, southwestern Saskatchewan and southeastern Alberta, Canada. Photograph courtesy of Erik Lizee from English Wikipedia. Effects of Groundwater Flow on the Distribution of Biogenic Gas in Parts of the Northern Great Plains of Canada and United States By Lawrence O. Anna Scientific Investigations Report 2010–5251 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2011 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Anna, L.O., 2011, Effects of groundwater flow on the distribution of biogenic gas in parts of the northern Great Plains of Canada and United States: U.S.
    [Show full text]
  • (Milk River) Strata Between the Hatton and Abbey-Lacadena Pools, Southwestern Saskatchewan – Preliminary Observations
    Stratigraphic Relationship of Alderson (Milk River) Strata Between the Hatton and Abbey-Lacadena Pools, Southwestern Saskatchewan – Preliminary Observations Per Kent Pedersen Pedersen, P.K. (2003): Stratigraphic relationship of Alderson (Milk River) strata between the Hatton and Abbey-Lacadena pools, southwestern Saskatchewan – preliminary observations; in Summary of Investigations 2003, Volume 1, Saskatchewan Geological Survey, Sask. Industry Resources, Misc. Rep. 2003-4.1, CD-ROM, Paper A-11, 11p. Abstract Large quantities of economically recoverable gas have recently been discovered within the Alderson Member of the Lea Park Formation in the Abbey-Lacadena pools. This occurrence, located approximately 50 km northeast of the prolific Hatton Pool, has sparked development within the area as well as exploration for similar plays elsewhere in southwestern Saskatchewan. Strata of the Alderson Member are commonly identified by industry and government geologists as belonging to the Milk River Formation. Recent research has indicated, however, that most of the Alderson strata are younger than strata of the Milk River Formation. Within the Abbey-Lacadena pools, the Alderson Member is composed of stacked, subtly upward-coarsening parasequences. Gas is hosted in thin, very fine-grained sandstone beds interbedded with silty mudstones. The sands likely were deposited in a storm- dominated, pro-delta setting below fair-weather wave base. The main productive sandstone is a composite lowstand unit, which both onlaps, and is overlain by, mudstones. Structural maps of the top of the Alderson Member (Milk River “shoulder”) show the Abbey-Lacadena area as a structural high. Thus, initial drilling indicates prolific gas production within the Abbey-Lacadena pools is closely related to the concurrence of a structural high and lowstand sandstones.
    [Show full text]
  • A Multidisciplinary Palaeoenvironmental Reconstruction of the Campanian Foremost Formation of Southern Alberta
    A Multidisciplinary Palaeoenvironmental Reconstruction of the Campanian Foremost Formation of Southern Alberta by Michael Glen Wenstob Thompson A thesis submitted to the Faculty of Graduate and Postdoctoral Affairs in partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences Carleton University Ottawa, Ontario © 2018, Michael Glen Wenstob Thompson Abstract The Foremost Formation of southern Alberta, Canada, is the basal member of the Cretaceous (Campanian) Belly River Group, and has been understudied relative to the overlying Oldman and Dinosaur Park formations of this group. Examined outcrop of the upper Foremost Formation preserves coastal estuarine or barrier island/lagoonal environments that transition upward into more inland coastal/ fluvial plain environments during the Claggett marine regression of the Western Interior Seaway. A low abundance, low diversity agglutinated benthic foraminiferal fauna, together with whole rock geochemical proxies, suggests commonly stressed oxygen and salinity conditions in marginal marine environments. Vertebrate microsite faunas display a primarily brackish water environmental influence, with an increase in diversity upsection in conjunction with increased terrestrial deposition. Hadrosaur remains suggest the previously unknown presence of kritosaurs and potentially a basal hadrosauroid, suggesting that the Foremost Formation dinosaur fauna was similarly diverse compared to faunas of well-characterized Campanian formations in North America. ii Acknowledgments My genuine thanks go out to Dr. Claudia Schröder-Adams and Dr. Michael Ryan for giving me the opportunity to work on such an exciting, multidisciplinary project and for their knowledge, advice, and encouragement throughout my time at Carleton University. I’d like to thank Kieran Shepherd and Margaret Currie at the Canadian Museum of Nature and Brandon Strilisky at the Royal Tyrrell Museum for allowing access to their institution’s vertebrate fossil collections and for the assistance they gave me during my research.
    [Show full text]
  • Palaeoecology of Vertebrate Assemblages from the Upper Cretaceous Judith River Group (Campanian) of Southeastern Alberta, Canada
    University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies Legacy Theses 1997 Palaeoecology of vertebrate assemblages from the Upper Cretaceous Judith River group (campanian) of southeastern Alberta, Canada Peng, Jianghua Peng, J. (1997). Palaeoecology of vertebrate assemblages from the Upper Cretaceous Judith River group (campanian) of southeastern Alberta, Canada (Unpublished doctoral thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/17933 http://hdl.handle.net/1880/26786 doctoral thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca THE UNIVERSITY OF CALGARY Palaeoecology Of Vertebrate Assemblages From The Upper Cretaceous Judith River Group (Campanian) Of Southeastern Alberta, Canada by Jianghua Peng A DISSERTATION SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY DEPARTMENT OF BIOLOGICAL SCIENCES CALGARY, ALBERTA DECEMBER, 1997 © Jianghua Peng 1997 The author of this thesis has granted the University of Calgary a non-exclusive license to reproduce and distribute copies of this thesis to users of the University of Calgary Archives. Copyright remains with the author. Theses and dissertations available in the University of Calgary Institutional Repository are solely for the purpose of private study and research. They may not be copied or reproduced, except as permitted by copyright laws, without written authority of the copyright owner.
    [Show full text]
  • THE FIRST MONODOMINANT HADROSAUR BONEBED from the OLDMAN FORMATION (CAMPANIAN) of ALBERTA by EVAN E. SCOTT Submitted in Partial
    THE FIRST MONODOMINANT HADROSAUR BONEBED FROM THE OLDMAN FORMATION (CAMPANIAN) OF ALBERTA by EVAN E. SCOTT Submitted in partial fulfillment of the requirements for the degree of Master of Science Department of Earth, Environmental, and Planetary Sciences CASE WESTERN RESERVE UNIVERSITY August, 2015 CASE WESTERN RESERVE UNIVERSITY SCHOOL OF GRADUATE STUDIES We hereby approve the thesis of Evan E. Scott candidate for the degree of Masters of Science*. Committee Chair Beverly Saylor Committee Member Peter McCall Committee Member Michael Ryan Date of Defense May 21, 2015 *We also certify that written approval has been obtained for any proprietary material contained therein. 2 TABLE OF CONTENTS 1. INTRODUCTION Project Rationale 11 Hadrosauridae 12 Bonebeds 14 Histology 17 2. MATERIALS AND METHODS Field Methods 22 Laboratory Methods 26 3. REGIONAL AND LOCAL GEOLOGY Regional Geology 28 Local Geology 29 4. CRANIAL AND POSTCRANIAL ANATOMY 32 5. TAPHONOMY Taxonomic Composition of Wendy’s Bone Bed 48 Taphonomic Modifications 48 Relative Age Profile of Wendy’s Bone Bed 54 6. HISTOLOGICAL DESCRIPTIONS 60 7. DISCUSSION Taphonomy 68 Histology 75 Histological Age Profile 77 Bone texture as a possible indicator of ontogenetic stage 80 Sociality 81 Conclusions 82 APPENDICES Appendix A: Histological Preparation 84 3 REFERENCES 89 4 TABLES Table 1. Summary of measurements and histological observations for sectioned WBB tibiae. 27 Table 2. Summary of taphonomic data. 53 5 FIGURES Figure 1. Representative histological cross section. 21 Figure 2. Map of southern Alberta and its geographic relationship to the rest of Canada. 23 Figure 3. Panorama of field locality. Inset: close-up of WBB quarry.
    [Show full text]