Allostratigraphy, Paleogeographic Evolution and Accommodation Controls of the Lower Colorado Allogroup in West-Central Alberta
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Abrupt Facies Changes Across a Flexural Depocentre
Stratigraphy and Sedimentology of the Peace River Formation: Abrupt Facies Changes across a Flexural Depocentre Robin Buckley* Department of Earth Sciences, University of Western Ontario London, Ontario, Canada N6A 5B7 [email protected] Jessica Krawetz Canadian Natural Resources Limited, Suite 2500, 855-2nd Street SW, Calgary, Alberta, T2P 4J8. and A. Guy Plint Department of Earth Sciences, University of Western Ontario London, Ontario, Canada, N6A 5B7 Abstract In northeastern British Columbia and northwestern Alberta, progradational shoreface sandstones of the Middle Albian Cadotte Member of the Peace River Formation are capped by a subaerial unconformity that defines the base of the Paddy Member. Towards the north, the clean, medium- to coarse-grained sandstones of the Cadotte Member pass laterally, over ~9 km, into hummocky cross-stratified (HCS) glauconitic sandstones interbedded with silty bioturbated mudstones. This facies transition trends ENE-WSW and can be mapped for over 180 km. The Paddy Member represents three main depositional environments: Coastal plain and brackish lagoonal deposits are represented by paleosols, mudstones with brackish- and freshwater molluscs, channel fills, crevasse splays and coals. These facies thicken and become progresssively more terrestrial towards the Foothills in the SW. Nonmarine deposits pass laterally northward into a belt of clean sandstone characterized by parallel lamination and cross bedding with Skolithos and Ophiomorpha suggestive of deposition in marine shoreface. The shoreface sandstones trend ENE-WSW and pass abruptly northward into heterolithic glauconitic sandstone and mudstone deposits typified by HCS and a Cruziana ichnofauna, indicative of a shallow shelf. The lateral facies change from shoreface sandstone into offshore HCS facies is similar in character, and parallel to that of the underlying Cadotte shoreface. -
Chapter Upper Cretaceous Reservoirs
CHAPTER 9 UPPER CRETACEOUS RESERVOIRS P. Viney, Petrel Robertson; Part B: Belly River Fm; and J.F. Chappell, L.L. & E. Canada; Part A: Cardium Fm INTRODUCTION The Bearpaw Fm, over 150 m thick in southcentral Alberta it would appear that exploration dollars directed towards them could Walker (1987, 1988), Swagor (1975) and Swagor et al. (1976). (14-18-2-23W4M), thins to the north and grades into the non-marine yield a good rate of return. Interest in exploration for these Cardium Fm conglomerate reser The evolution of the Alberta Basin during Upper Cretaceous time sequence of the overlying Horseshoe Canyon Fm (Edmonton Gp). voirs was reactivated in the early 1980's due to the discovery of and its effect on the geologic section is covered in the introduction to The four major Upper Cretaceous reservoirs are: 1) The Cardium; several new Cardium Fm pools and the recognition that modern this text. Strata of the Upper Cretaceous underlie most of the area Production has been obtained from the Upper Cretaceous section 2) The lower Belly River; 3) The Dunvegan-Doe Creek; and 4) The seismic reflection technology could be used in their detection covered by the Western Canada Sedimentary Basin in an almost con for many years. However, prospecting for Upper Cretaceous hydro Belly River fluvial. (Chappell, 1984, 1985; Wren, 1984). The Carrot Creek Cardium S tinuous sequence of deposition. From the Base of Fish Scales Zone, carbons did not begin in earnest until the discovery of Cardium pool, located in 53-12 and 13 W5M (Fig. 9.4), is a typical example. -
Mannville Group of Saskatchewan
Saskatchewan Report 223 Industry and Resources Saskatchewan Geological Survey Jura-Cretaceous Success Formation and Lower Cretaceous Mannville Group of Saskatchewan J.E. Christopher 2003 19 48 Printed under the authority of the Minister of Industry and Resources Although the Department of Industry and Resources has exercised all reasonable care in the compilation, interpretation, and production of this report, it is not possible to ensure total accuracy, and all persons who rely on the information contained herein do so at their own risk. The Department of Industry and Resources and the Government of Saskatchewan do not accept liability for any errors, omissions or inaccuracies that may be included in, or derived from, this report. Cover: Clearwater River Valley at Contact Rapids (1.5 km south of latitude 56º45'; latitude 109º30'), Saskatchewan. View towards the north. Scarp of Middle Devonian Methy dolomite at right. Dolomite underlies the Lower Cretaceous McMurray Formation outcrops recessed in the valley walls. Photo by J.E. Christopher. Additional copies of this digital report may be obtained by contacting: Saskatchewan Industry and Resources Publications 2101 Scarth Street, 3rd floor Regina, SK S4P 3V7 (306) 787-2528 FAX: (306) 787-2527 E-mail: [email protected] Recommended Citation: Christopher, J.E. (2003): Jura-Cretaceous Success Formation and Lower Cretaceous Mannville Group of Saskatchewan; Sask. Industry and Resources, Report 223, CD-ROM. Editors: C.F. Gilboy C.T. Harper D.F. Paterson RnD Technical Production: E.H. Nickel M.E. Opseth Production Editor: C.L. Brown Saskatchewan Industry and Resources ii Report 223 Foreword This report, the first on CD to be released by the Petroleum Geology Branch, describes the geology of the Success Formation and the Mannville Group wherever these units are present in Saskatchewan. -
TGI Strat Column 2009.Cdr
STRATIGRAPHIC CORRELATION CHART TGI II: Williston Basin Architecture and Hydrocarbon Potential in Eastern Saskatchewan and Western Manitoba EASTERN MANITOBA PERIOD MANITOBA SUBSURFACE SASKATCHEWAN OUTCROP ERA glacial drift glacial drift glacial drift Quaternary Wood Mountain Formation Peace Garden Peace Garden Member Tertiary Member Ravenscrag Formation CENOZOIC Formation Goodlands Member Formation Goodlands Member Turtle Mountain Turtle Mountain Turtle Frenchman Formation Whitemud Formation Boissevain Formation Boissevain Formation Eastend Formation Coulter Member Coulter Member Bearpaw Formation Odanah Member Belly River “marker” Odanah Member Belly River Formation “lower” Odanah Member Millwood Member Lea Park Formation Millwood Member MONTANA GROUP Pembina Member Pembina Member Pierre Shale Pierre Shale Milk River Formation Gammon Ferruginous Member Gammon Ferruginous Member Niobrara Formation Chalky Unit Boyne Member Boyne Member Boyne Calcareous Shale Unit Member Carlile Morden Member Carlile upper Formation Morden Member Formation Morden Member Carlile Formation Assiniboine Marco Calcarenite Assiniboine Member Member CRETACEOUS Second White Specks Laurier Limestone Beds Favel Favel Keld Keld Member Member Formation Formation Belle Fourche Formation Belle Fourche Member MESOZOIC COLORADO GROUP Belle Fourche Member upper Fish Scale Formation Fish Scale Zone upper Base of Fish Scale marker Base of Fish Scale marker Westgate Formation Westgate Member lower Westgate Member Newcastle Formation Newcastle Member lower Viking Sandstone -
Petroleum System Modeling of the Western Canada Sedimentary Basin – Isopach Grid Files
Petroleum System Modeling of the Western Canada Sedimentary Basin – Isopach Grid Files By Debra K. Higley1, Mitchell E. Henry, and Laura N.R. Roberts Report Series 2005-1421 U.S. Department of the Interior U.S. Geological Survey 1 Inquiries about this publication should be addressed to: Debra K. Higley U.S. Geological Survey, MS 939, Box 25046 Denver Federal Center, Denver, CO 80225 Tel: 303-236-5791 Email: [email protected] 1 U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia 2005 For products and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS–the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Debra K. Higley, Mitchell Henry, and Laura N.R. Roberts, 2006, Petroleum System Modeling of the Western Canada Sedimentary Basin – Isopach Grid Files: U.S. Geological Survey Report Series 2005-1421, web publication and associated data files. 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 material contained within this report. 2 Contents Introduction …………………………………………………………….. 3 Data Processing Steps …………………………………………….……. 4 Acknowledgments ………………………………….………………..…. 5 Zmap-Format Grid Files ..………………………….………………..…. 5 References and Software Cited …………………….……………..……. -
Stratigraphjc, Diagenetic and Geochemical Study of Cretaceous Strata In
StratigraphJc, Diagenetic and Geochemical Study of Cretaceous Strata in Central Saskatchewan A thesis Submitted to the Faculty of Graduate Studies and Research In Partial Fulfillment of the Requirements For the Degree of Master of Science In Geology University of Regina by Autumn Q Wang Regina, Saskatchewan August, 2010 Copyright 2010: Autumn Q. Wang Library and Archives Bibliotheque et 1*1 Canada Archives Canada Published Heritage Direction du Branch Patrimoine de I'edition 395 Wellington Street 395, rue Wellington OttawaONK1A0N4 OttawaONK1A0N4 Canada Canada Your file Votre reference ISBN: 978-0-494-79906-2 Our file Notre reference ISBN: 978-0-494-79906-2 NOTICE: AVIS: The author has granted a non L'auteur a accorde une licence non exclusive exclusive license allowing Library and permettant a la Bibliotheque et Archives Archives Canada to reproduce, Canada de reproduire, publier, archiver, publish, archive, preserve, conserve, sauvegarder, conserver, transmettre au public communicate to the public by par telecommunication ou par I'Internet, prefer, telecommunication or on the Internet, distribuer et vendre des theses partout dans le loan, distribute and sell theses monde, a des fins commerciales ou autres, sur worldwide, for commercial or non support microforme, papier, electronique et/ou commercial purposes, in microform, autres formats. paper, electronic and/or any other formats. The author retains copyright L'auteur conserve la propriete du droit d'auteur ownership and moral rights in this et des droits moraux qui protege cette these. Ni thesis. Neither the thesis nor la these ni des extraits substantiels de celle-ci substantial extracts from it may be ne doivent etre imprimes ou autrement printed or otherwise reproduced reproduits sans son autorisation. -
A Study of Potential Co-Product Trace Elements Within the Clear Hills Iron Deposits, Northwestern Alberta
Special Report 08 A Study of Potential Co-Product Trace Elements Within the Clear Hills Iron Deposits, Northwestern Alberta NTS 83M,N, 84C,D A STUDY OF POTENTIAL CO-PRODUCT TRACE ELEMENTS WITHIN THE CLEAR HILLS IRON DEPOSITS, NORTHWESTERN ALBERTA Prepared for Research and Technology Branch, Alberta Energy Prepared by APEX Geoscience Ltd. (Project 97213) In cooperation with The Alberta Geological Survey, Energy and Utility Board And Marum Resources Ltd. February, 1999 R.A. Olson D. R. Eccles C.J. Collom A STUDY OF POTENTIAL CO-PRODUCT TRACE ELEMENTS WITHIN THE CLEAR HILLS IRON DEPOSITS, NORTHWESTERN ALBERTA TABLE OF CONTENTS SECTION PAGE ACKNOWLEDGMENTS AND DISCLAIMER ....................................................... vi 1.0 SUMMARY ........................................................................................................1 2.0 INTRODUCTION ..................................................................................................3 2.1 Preamble....................................................................................................3 2.2 Location, Access, Physiography, Bedrock Exposure .................................4 2.3 Synopsis of Prior Scientific Studies of the Clear Hills Iron Deposits, and the Stratigraphically Correlative Bad Heart Formation ...............................4 2.4 Synopsis of Prior Exploration of the Clear Hills Iron Deposits....................6 3.0 GEOLOGY ........................................................................................................7 3.1 Introduction -
Cadomin and Jasper Areas Willem Langenberg and John Waldron
Field Guide to Selected Geological Sections of the Cadomin and Jasper Areas Willem Langenberg and John Waldron Edmonton Geological Society Field Trip Guide September 22-23, 2007 Introduction The Rocky Mountains can be divided into Foothills, Front Ranges, and Main Ranges as shown in the cartoon below (Fig. 1). Outcrops in the foothills are dominated by softer weathering Mesozoic rocks of the foreland basin: mainly sandstone and shale but also including conglomerates and coal. Most of the clastic rocks represent material eroded from earlier-formed parts of the orogen to the west, which was subsequently cannibalized as the thrustbelt advanced westward in late Mesozoic to early Cenozoic time. Locally in the foothills, the more resistant late Paleozoic carbonate rocks come to the surface in elongated ridges. Saturday's traverse will begin in the foothills of the Cadomin area and proceed southwest into the Front Ranges. In the Front Ranges carbonates dominate the landscape. These represent the late Paleozoic continental margin of the Laurentian continent, now sliced into multiple imbricated thrust sheets. Mesozoic clastics are confined to narrow valleys. On Sunday morning we will take the Yellowhead Highway further into the Front Ranges and eventually into the Main Ranges of the Rockies. In the Main Ranges, lower parts of the stratigraphy are preserved, including widespread outcrops of older, Early Paleozoic carbonates, clastics, and the underlying Proterozoic succession of the Windermere Supergroup. The structural style is different, too. Although thrust sheets are present, they are generally much larger in scale, and their dips are gentler. In addition, the rocks were more ductile when deformed, so that cleavage and folds are much more widely developed in the mudrocks. -
The Viking Formation (Lower Cretaceous) of Southeastern Saskatchewan
University of Windsor Scholarship at UWindsor Electronic Theses and Dissertations Theses, Dissertations, and Major Papers 1-1-1981 The Viking Formation (Lower Cretaceous) of southeastern Saskatchewan. Shaun C. O'Connell University of Windsor Follow this and additional works at: https://scholar.uwindsor.ca/etd Recommended Citation O'Connell, Shaun C., "The Viking Formation (Lower Cretaceous) of southeastern Saskatchewan." (1981). Electronic Theses and Dissertations. 6773. https://scholar.uwindsor.ca/etd/6773 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. NOTE TO USERS This reproduction is the best copy available. UMI_ (B) Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. THE VIKING FORMATION (LOWER CRETACEOUS) OF SOUTHEASTERN SASKATCHEWAN by Shaun C. O' Connell Thesis Submitted to the Faculty of Graduate Studies through the Department of Geology in Partial Fulfilment of the Requirements for the degree of Master of Science in Geology at The University of Windsor. -
Exploration Analysis
EXPLORATION ANALYSIS CARDIUM FORMATION Current Situation The Cardium Formation is not an exploration target in B.C. Where it has been tested, it is as a secondary target, and often with a straddle drillstem test run on the basis of a prospective well log signature. The formation has thus been open to drilling fluids for an extended period of time, and wellbore damage is likely to be severe. This situation is exacerbated by lack of reservoir “sweet spots”, shallow drilling depths and subnormal formation pressures. Velvet Exploration undertook an exploration program in 2000/2001 for fractured Cardium shoreface sandstones in the Copton-Narraway area of Alberta, in the southeastern corner of Map 2. There do not appear to be a substantial number of new Cardium wells on production in this area, and Velvet’s successor, El Paso, is not drilling new wells on the play. Tight Gas Potential The Cardium presents an attractive in-place gas resource, with massive sandstones of substantial thickness distributed continuously over a large area (Map 2) (Table 1). Because of its shallow burial depth, there has been less reservoir degradation by compaction than for deeper tight gas reservoirs. However, low reservoir pressures reduce in-place gas volumes, particularly within the subnormally-pressured Deep Basin. By qualitative comparison with the Cadotte and Spirit River, we speculate an in-place gas resource of 1-3 BCF/section. Cardium tight gas will likely be a secondary, uphole target to be exploited in conjunction with deeper tight gas plays. Locally, Cardium gas production may occur where: • operators stumble upon conglomeratic sweet spots, or • fracture-enhanced reservoir sections are defined in the Foothills, where the Cardium section is thickest. -
Dynamic Sedimentation in the Late Albian, South-Central Alberta and Saskatchewan Matea Drljepan.; A
Dynamic sedimentation in the Late Albian, south-central Alberta and Saskatchewan Matea Drljepan.; A. Guy Plint University of Western Ontario Summary Across southern Alberta and Saskatchewan, rocks of Late Albian age (including the Joli Fou, Viking, Bow Island and Mill Creek formations) represent depositional environments ranging from alluvial to deltaic- nearshore to offshore marine. Because of radical facies changes, it is difficult to establish age relationships amongst these various lithostratigraphic formations. Building upon an existing allostratigraphic framework developed by Boreen and Walker (1991), Roca et al. (2008), Buckley and Plint (2013), and Vannelli (2016) have modified the original allostratigraphic scheme and extended correlation of Upper Albian strata to northern Alberta and NE British Columbia. The investigation reported here builds upon these allostratigraphic studies and extends across 56,000 km2 of south-central Alberta and Saskatchewan. Preliminary results show that early Late Albian Joli Fou sediments form a subtly SE- thickening wedge whereas lower Viking allomembers VA and VB are approximately sheet-like, with local thickening to the SW reflecting local deltaic depocentres. Viking allomember VD contasts markedly with allomembers VA and VB because it forms a prominent, elongate SW-thickening wedge that extends across Alberta into Saskatchewan, within which, parasequences onlap towards the NE. The NE limit of the wedge is abrupt, defined by a prominent lineament, or hinge-line. To the south of the hinge, overlapping sandy deltaic lobes can be mapped whereas to the north of the hinge, the rocks are mudstone-dominated. Introduction The Viking Formation represents one of the most prolific hydrocarbon reservoirs in the Western Canada Foreland Basin, containing 5 to 8% of the total oil in Alberta (Reinson et al., 1994) and a total estimated oil reserve of 88.7 million m3 (Alberta Research Council et al., 1994). -
Quaternary Stratigraphy and Surficial Geology Peace River Final Report
SPE 10 Quaternary Stratigraphy and Surficial Geology Peace River Final Report Alberta Energy and Utilities Board Alberta Geological Survey QUATERNARY STRATIGRAPHY AND SURFICIAL GEOLOGY PEACE RIVER - FINAL REPORT Alberta Geological Survey Special Report SPE10 (Canada – Alberta MDA Project M93-04-035) Prepared by L.E. Leslie1 and M.M. Fenton Alberta Energy and Utilities Board Alberta Geological Survey Branch 4th Floor Twin Atria Building 4999 98 Avenue Edmonton, Alberta T6B 2X3 Release date: January 2001 (1)Geo-Environmental Ltd., 169 Harvest Grove Close NE , Calgary AB T3K 4T6 ACKNOWLEDGEMENTS The authors wish to thank Dr. B. Garrett (Geological Survey of Canada) for providing a GSC till standard to use as controls in geochemical analyses of the samples submitted to various laboratories during this study. Thanks also to R. Richardson and R. Olson for reviewing the manuscript and T. Osachuk and D. Troop of Prairie Farm Rehabilitation Administration regarding the Grimshaw groundwater report. The co-operation and assistance received from the personnel at Municipal Districts of 22, 131 and 135, the Peace River Alberta Transportation Regional office is sincerely appreciated. The various companies involved in locating subsurface utilities conducted through Alberta First Call were completed efficiently and without delay The writers are indebted to the willing and able support from the field assistants Solweig Balzer (1993), Nadya Slemko (1994) and Joan Marklund (1995). Special thanks also goes to Dan Magee who drafted the coloured surficial geology map. Partial funding for field support in 1994 was provided by a grant from the Canadian Circumpolar Institute. i PREFACE This report is one of the final products from a project partly funded under the Canada- Alberta Partnership Agreement on Mineral Development (Project M93-04-035) through the Mineral Development Program by what was then called the Alberta Department of Energy (now Department of Resource Development).