Alberta Basin. See Western Canada Foreland Basin. Alexander Terrane
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MAY 2014 VOLUME 41, ISSUE 05 Canadian Publication Mail Contract – 40070050 MORE THAN MAPPING WANT to LIFT YOUR PETREL® WORKFLOWS to NEW HEIGHTS?
20 Fossils Hunting for Provinces 28 Go Take a Hike 34 GeoConvention 2014: Focus 36 Bringing the Cretaceous Sea to Mount Royal University: A Proposal to Fund the East Gate Entrance Fossil Display $10.00 MAY 2014 VOLUME 41, ISSUE 05 Canadian Publication Mail Contract – 40070050 MORE THAN MAPPING WANT TO LIFT YOUR PETREL® WORKFLOWS TO NEW HEIGHTS? Seamlessly bring more data into the fold. Dynamically present your insight like never before. SOFTWARE SERVICES CONNECTIVITY DATA MANAGEMENT The Petrosys Plug-in for Petrel® gives you access to powerful Petrosys mapping, surface modeling and data exchange from right where you need it – inside Petrel. Now you have the power to effortlessly and meticulously bring your critical knowledge together on one potent mapping canvas. Work intuitively with your Petrel knowledge and, should you so require, simultaneously aggregate, map and model data direct from multiple other sources – OpenWorks®, ArcSDE®, IHS™ Kingdom®, PPDM™ and more. Refine, enhance and then present your results in beautiful, compelling detail. The result? Decision-making is accelerated through consistent mapping and surface modeling as focus moves from regional overview through to the field and reservoir scale. To learn more go to www.petrosys.com.au/petrel. Petrel is a registered trademark of Schlumberger Limited and/or its affiliates. OpenWorks is a registered trademark of Halliburton. ESRI trademarks provided under license from ESRI. IHS and Kingdom are trademarks or registered trademarks of IHS, Inc. PPDM is a trademark of the Professional Petroleum Data Management (PPDM) Association. MAY 2014 – VOLUME 41, ISSUE 05 ARTICLES Fossils Hunting for Provinces ..................................................................................................... 20 CSPG OFFICE Tools to Tackle the Riddle of the Sands ............................................................................... -
Aplodontid, Sciurid, Castorid, Zapodid and Geomyoid Rodents of the Rodent Hill Locality, Cypress Hills Formation, Southwest Saskatchewan
APLODONTID, SCIURID, CASTORID, ZAPODID AND GEOMYOID RODENTS OF THE RODENT HILL LOCALITY, CYPRESS HILLS FORMATION, SOUTHWEST SASKATCHEWAN A Thesis Submitted to the College of Graduate Studies and Research in Partial Fulfillment of the Requirements for the Degree of Master of Science in the Department of Geological Sciences University of Saskatchewan Saskatoon By Sean D. Bell © Copyright Sean D. Bell, December 2004. All rights reserved. PERMISSION TO USE In presenting this thesis in partial fulfilment of the requirements for a Master’s degree from the University of Saskatchewan, I agree that the libraries of the University of Saskatchewan may make it freely available for inspection. I further agree that permission for copying of this thesis in any manner, in whole or in part, for scholarly purposes may be granted by the professors who supervised my thesis work or, in their absence, by the Head of the Department of Geological Sciences or the Dean of the College of Graduate Studies and Research. It is understood that any copying or publication or use of this thesis or parts thereof for financial gain shall not be allowed without my written permission. It is also understood that due recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis. Requests for permission to copy or to make other use of material in this thesis in whole or part should be addressed to: Head of the Department of Geological Sciences 114 Science Place University of Saskatchewan Saskatoon, Saskatchewan S7N 5E2 i ABSTRACT The Rodent Hill Locality is a fossil-bearing site that is part of the Cypress Hills Formation, and is located roughly 15 km northwest of the town of Eastend, Saskatchewan. -
Ecosystem-Based Management Plan for Cypress Hills Interprovincial Park
Cypress Hills Interprovincial Park ECOSYSTEM-BASED MANAGEMENT PLAN Saskatchewan.ca Ecosystem-Based Management Plan February 19, 2020 Cypress Hills Interprovincial Park ECOSYSTEM-BASED MANAGEMENT PLAN PROJECT REFERENCE NUMBER: 1467-5 March 11, 2020 Revised: March 2021 Prepared for: Saskatchewan Ministry of Parks, Culture and Sport 3211 Albert St Regina, SK S4S 5W6 Cypress Hills Interprovincial Park Page | 1 Approval Form The Ecosystem-based Management Plan for Cypress Hills Interprovincial Park (2020) is hereby approved for use by the Ministry of Parks, Culture and Sport in the management of the ecosystem and landscape of Cypress Hills Interprovincial Park. March 11, 2020 Darryl Sande, RPF, Plan Author Date FORSITE Inc. Recommended for approval by: March 1, 2021 Thuan Chu, Senior Park Landscape Ecologist Date Landscape Protection Unit Ministry of Parks, Culture and Sport Cypress Hills Interprovincial Park Page | ii EXECUTIVE SUMMARY Cypress Hills Interprovincial Park (CHIPP) is a 183 square kilometre Natural Environment Park within the southwestern corner of Saskatchewan. The park encompasses the unique geological features and elevation of the Cypress Hills formation. The area contains a mix of Boreal and Montane forest elements as well as Prairie grassland elements. The area is surrounded by agricultural and pasture lands. The park is made up of a mix of natural forests and grasslands, which is classified into nine ecosites. Upland ecosites include plains rough fescue grassland on silty clay loam, lodgepole pine-dominated stands on sandy clay, white spruce stands on silty clay, aspen stands on clay loam, aspen-white spruce mixedwoods on silty clay soils, and aspen-lodgepole pine mixedwoods on clay loam. -
Fluid Compartmentalization of Devonian and Mississippian Dolostones, Western Canada Sedimentary Basin: Evidence from Fracture Mineralization
University of Windsor Scholarship at UWindsor Electronic Theses and Dissertations Theses, Dissertations, and Major Papers 2016 Fluid Compartmentalization of Devonian and Mississippian Dolostones, Western Canada Sedimentary Basin: Evidence from Fracture Mineralization Carole Mrad University of Windsor Follow this and additional works at: https://scholar.uwindsor.ca/etd Recommended Citation Mrad, Carole, "Fluid Compartmentalization of Devonian and Mississippian Dolostones, Western Canada Sedimentary Basin: Evidence from Fracture Mineralization" (2016). Electronic Theses and Dissertations. 5752. https://scholar.uwindsor.ca/etd/5752 This online database contains the full-text of PhD dissertations and Masters’ theses of University of Windsor students from 1954 forward. These documents are made available for personal study and research purposes only, in accordance with the Canadian Copyright Act and the Creative Commons license—CC BY-NC-ND (Attribution, Non-Commercial, No Derivative Works). Under this license, works must always be attributed to the copyright holder (original author), cannot be used for any commercial purposes, and may not be altered. Any other use would require the permission of the copyright holder. Students may inquire about withdrawing their dissertation and/or thesis from this database. For additional inquiries, please contact the repository administrator via email ([email protected]) or by telephone at 519-253-3000ext. 3208. Fluid Compartmentalization of Devonian and Mississippian Dolostones, Western Canada Sedimentary -
The Letters F and T Refer to Figures Or Tables Respectively
INDEX The letters f and t refer to figures or tables respectively "A" Marker, 312f, 313f Amherstberg Formation, 664f, 728f, 733,736f, Ashville Formation, 368f, 397, 400f, 412, 416, Abitibi River, 680,683, 706 741f, 765, 796 685 Acadian Orogeny, 686, 725, 727, 727f, 728, Amica-Bear Rock Formation, 544 Asiak Thrust Belt, 60, 82f 767, 771, 807 Amisk lowlands, 604 Askin Group, 259f Active Formation, 128f, 132f, 133, 139, 140f, ammolite see aragonite Assiniboia valley system, 393 145 Amsden Group, 244 Assiniboine Member, 412, 418 Adam Creek, Ont., 693,705f Amundsen Basin, 60, 69, 70f Assiniboine River, 44, 609, 637 Adam Till, 690f, 691, 6911,693 Amundsen Gulf, 476, 477, 478 Athabasca, Alta., 17,18,20f, 387,442,551,552 Adanac Mines, 339 ancestral North America miogeocline, 259f Athabasca Basin, 70f, 494 Adel Mountains, 415 Ancient Innuitian Margin, 51 Athabasca mobile zone see Athabasca Adel Mountains Volcanics, 455 Ancient Wall Complex, 184 polymetamorphic terrane Adirondack Dome, 714, 765 Anderdon Formation, 736f Athabasca oil sands see also oil and gas fields, Adirondack Inlier, 711 Anderdon Member, 664f 19, 21, 22, 386, 392, 507, 553, 606, 607 Adirondack Mountains, 719, 729,743 Anderson Basin, 50f, 52f, 359f, 360, 374, 381, Athabasca Plain, 617f Aftonian Interglacial, 773 382, 398, 399, 400, 401, 417, 477f, 478 Athabasca polymetamorphic terrane, 70f, Aguathuna Formation, 735f, 738f, 743 Anderson Member, 765 71-72,73 Aida Formation, 84,104, 614 Anderson Plain, 38, 106, 116, 122, 146, 325, Athabasca River, 15, 20f, 35, 43, 273f, 287f, Aklak -
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 -
A Guide for Identifying Common Rock and Fossil Specimens Found in Saskatchewan Museums
A GUIDE FOR IDENTIFYING COMMON ROCK AND FOSSIL SPECIMENS FOUND IN SASKATCHEWAN MUSEUMS By: Frank H. McDougall 2015 Crinoid stem in Ordovician limestone FOREWARD The following guide was developed by the author in order to compliment the Saskatchewan Archaeology Societies (SAS) summer archaeological caravan tours that began in 2012 and has visited many local Saskatchewan museums. The author has drawn on an extensive career in mining exploration and palaeontology as well as experience with local provincial museum collections in preparing this guide. This document is designed to aid local museums to identify some of the rock and fossil specimens that they contain. It is not meant to be an exhaustive resource that will allow the user to identify all specimens as museums often contain many unusual and unique specimens. It does however attempt to cover many of the specimens of rocks and fossils that are commonly found in local provincial museum collections. The guide is laid out in two main sections. The first section deals with identifying common rock specimens while the second section deals with common fossil specimens. A Guide for Identifying Common Rock and Fossil Specimens for Saskatchewan Museums i TABLE OF CONTENTS FOREWARD ....................................................................................................................... i TABLE OF CONTENTS.................................................................................................... ii LIST OF FIGURES ........................................................................................................... -
National Park Service Paleontological Research
169 NPS Fossil National Park Service Resources Paleontological Research Edited by Vincent L. Santucci and Lindsay McClelland Technical Report NPS/NRGRD/GRDTR-98/01 United States Department of the Interior•National Park Service•Geological Resource Division 167 To the Volunteers and Interns of the National Park Service iii 168 TECHNICAL REPORT NPS/NRGRD/GRDTR-98/1 Copies of this report are available from the editors. Geological Resources Division 12795 West Alameda Parkway Academy Place, Room 480 Lakewood, CO 80227 Please refer to: National Park Service D-1308 (October 1998). Cover Illustration Life-reconstruction of Triassic bee nests in a conifer, Araucarioxylon arizonicum. NATIONAL PARK SERVICE PALEONTOLOGICAL RESEARCH EDITED BY VINCENT L. SANTUCCI FOSSIL BUTTE NATIONAL MONUMNET P.O. BOX 592 KEMMERER, WY 83101 AND LINDSAY MCCLELLAND NATIONAL PARK SERVICE ROOM 3229–MAIN INTERIOR 1849 C STREET, N.W. WASHINGTON, D.C. 20240–0001 Technical Report NPS/NRGRD/GRDTR-98/01 October 1998 FORMATTING AND TECHNICAL REVIEW BY ARVID AASE FOSSIL BUTTE NATIONAL MONUMENT P. O . B OX 592 KEMMERER, WY 83101 164 165 CONTENTS INTRODUCTION ...............................................................................................................................................................................iii AGATE FOSSIL BEDS NATIONAL MONUMENT Additions and Comments on the Fossil Birds of Agate Fossil Beds National Monument, Sioux County, Nebraska Robert M. Chandler .......................................................................................................................................................................... -
Back Matter (PDF)
Index adsorption 15-16 Caithness Flags 168 adsorption chromatography 152, 153 Canada see Nova Scotia Basin also Western Canada Age anticline 243 Sedimentary Basin Alabama see Mexican Gulf Coast carbon dioxide and migration 156 Alberta 218 carbon isotope ratios 193, 195 Alpine foreland carbon mass balance 11 maturation Carboniferous temperature 240-1 reservoirs 35, 41, 42, 218 timing 238-40 source rocks 210 regional setting 227-9 Cardium Formation 124, 209, 216 regional studies cataclasis v. diffusive mass transfer 256 Clergeon anticline 232-5 Central Graben (North Sea) see also Sub-Alpine Chains compaction studies 70-2, 76-9 stratigraphy 230-1 migration studies 52, 175, 177 structure 229 Charlie Lake Formation 209, 210 subsidence history 231-2 Chinchaga-Contact Rapids Formation 212 thrust timing 231 chromatography alteration v. degradation 197 fractionation 144, 145 Alwyn kitchen 91 process applications 152-4 Andrade formula 107 gas-liquid 156-7 Annecy 227, 241,246 gas-solid 156 aqueous fractionation 200, 201-2 liquid-liquid 155-6 aquifer properties 128, 130 liquid-solid 154-5 Arbuckle Formation 201 quantification 157-9 Are Formation 273 results 198 Arkansas 52 techniques 151-2 see also Mexican Gulf Coast theory 150-1 asphalt 227, 241,246 clay minerals Athabasca tar sands 208, 216 adsorption 15-16 Australia case study 24-7 permeability 12-13 Clergeon anticline 229, 232 burial history 232-4 Bakken Shale Formation 51-2 thermal history 234-5 Balder field 178 coal Baider Sandstone 183 oleophilicity 16 Banff Group 209 source potential 23-4 -
Induced Seismicity Study in the Kiskatinaw Seismic Monitoring and Mitigation Area, British Columbia for the BC Oil and Gas Commission
Induced Seismicity Study in the Kiskatinaw Seismic Monitoring and Mitigation Area, British Columbia for the BC Oil and Gas Commission Amy D. Fox, Ph.D., P. Geo. and Neil D. Watson, P. Geol. Final Report June 5, 2019 Disclaimer All work performed for this project and information provided in this report is of the highest technical quality possible given data limitations and uncertainties at the time the work was completed. Enlighten Geoscience Ltd. cannot guarantee the accuracy of the material included in this report (and corresponding presentation) and bears no responsibility for the use of the material. This report was written as a preliminary contribution to understanding issues surrounding induced seismicity in the Kiskatinaw Seismic Monitoring and Mitigation Area. The ability to predict induced seismicity or infer economic valuations is explicitly not meant to be implied from this report. Enlighten Geoscience Ltd. APEGA Permit P13351 Member #159887 June 5, 2019 © 2019 Enlighten Geoscience Ltd. 2 Executive Summary Induced seismicity has been a growing concern throughout North America and around the world as increasing numbers of seismic events have been occurring in historically quiet tectonic areas and appear to be related to localized oil and gas development activity. On November 29, 2018 hydraulic fracture operations were suspended after a series of three seismic events ranging from 3.4 to 4.5 magnitude were recorded in the Kiskatinaw Seismic Monitoring and Mitigation Area (KSMMA) in northeast British Columbia, Canada. The goal of this study was to perform the first phase of a larger investigation designed to identify key or common factors coincident with induced seismicity and/or to delineate areas of higher induced seismicity likelihood within the KSMMA. -
Alberta T2L 2A7
GEOLOGICAL SURVEY OF CANADA COMMISSION GEOLOGIQUE DU CANADA Podruski, J.A., Barc Canadz , I GEOLOGICAL SURVEY OF CANADA PAPER 87-26 CONVENTIONAL OIL RESOURCES OF WESTERN CANADA (LIGHT AND MEDIUM) PART I: RESOURCE ENDOWMENT Podruski, J.A., Barclay, J.E., Hamblin, A.P., Lee, P.J., Osadetz, K.G., Procter, R.M., and Taylor, G.C. PART II: ECONOMIC ANALYSIS Conn, R.F., and Christie, J.A. @Minister of Supply and Services Canada 1987 Available in Canada through authorized book store agents and other book stores or by mail from Canadian Government Publishing Centre Supply and Services Canada Hull, Quebec, Canada KIA OS9 and from Geological Survey of Canada 601 Booth Street Ottawa, Canada KIA OE8 and Institute of Sedimentary and Petroleum Geology Geological Survey of Canada 3303 - 33rd Street, N.W. Calgary, Alberta T2L 2A7 A deposit copy of this publication is also available for reference in public libraries across Canada Cat. No. M44-87126E Canada: $10.00 ISBN 0-660-1 2650-8 Other Countries: $1 2.00 Price subject to change without notice Scientific Editor P. Fitzgerald-Moore Production manager L. Mac Lachlan Layout and artwork supervised by I. W. Thomson W. P. Vermette Typesetting supervised by P. L. Greener Cartography and Word Processing units Institute of Sedimentary and Petroleum Geology Authors' addresses Podruski, /.A,, Barclay, j.E., Hamblin, A.P., Lee, P.]., Osadetz, K.C., Procter, R.M., and Taylor, C.C. Institute of Sedimentary and Petroleum Geology 3303 - 33rd Street, N.W., Calgary, Alberta T2L 2A7 Conn, R.F., and Christie, ).A. Petroleum Resources Branch Energy, Mines and Resources 580 Booth Street, Ottawa, Ontario KIA 0E4 Cette publication est aussi disponible en francais PREFACE The major oil discovery at Leduc in 1947 led to the develop La decouverte majeure de petrole faite A Leduc en 1947 a men6 h I'essor ment of a vital Canadian petroleum industry. -
The Cypress Hills Gravel
Appendix 6 The Cypress Hills Gravel The Cypress Hills are a broad, eastward-extending anticline 1 that has been planed on generally horizontal sedimentary rocks. In a few locations, the Cypress Hills planation surface bevels dipping sedimentary rocks. 2 Steep slopes separate the plateau from the plains to the north. To the south a “pediment-like” planation surface slopes gently away from the plateau3,4,5 to the level of the plains. The plains are also a generally flat plana- tion surface (the Flaxville planation surface) with occasional beveling of the sedimentary rocks.6 Pediments are one of the geomorphological subjects of volume III. Predominantly Quartzite Gravel from the Rocky Mountains The gravel or conglomerate capping the Cypress Hills is weakly stratified, poorly sorted, imbricated, and clast supported.7,8,9,10 The western and central Cypress Hills have a few fine-grained interbeds. Gravel in the western area lies on the Ravenscrag Forma- tion (locally it lies on the Frenchman Formation) which consists mostly of soft silt and clay with minor cross-bedded sandstone.1,11 Lozenge-shaped sandstone rocks from these formations are sometimes found within the Cypress Hills Formation.1 The Cypress Hills gravel rests on a slightly uneven planation surface with a relief of less than 50 feet (15 m).10 In the eastern Cypress Hills, the coarse gravel is estimated up to 245 feet (75 m) 1 Furnival, G.M., 1950. Cypress Lake map-area, Saskatchewan. Geological Survey of Canada Memoir 242, Canada Department of Mines and Technical Surveys, Ottawa, Canada. 2 Williams, M.Y.