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The Duvernay Resource
AB & BC Montney Technical Session Thursday, February 20th, 2020 801 Seventh +15 – 667 7 Street SW THANK YOU TO OUR SPONSORS! AB & BC Montney Day An Update on AB and BC’s Montney Resource Play February 20th, 2020 AB & BC Montney Technical Session Thursday, February 20th, 2020 801 Seventh +15 – 667 7 Street SW QUESTIONS & ANSWERS FORMAT For this workshop, we will use CSUR`s website to make it easy for everyone to share their ideas, opinions and most importantly, questions! How it works: 1) Go to our website through the respective link: Montney Overview Session visit: https://www.csur.com/question/mo Technical Session #1 Session visit: https://www.csur.com/question/1 Technical Session #2 Session visit: https://www.csur.com/question/2 Technical Session #3 Session visit: https://www.csur.com/question/3 2) Submit your question and it will be displayed on the screen 3) Please note that “write your answer” is where you should write your question and submit your answer will complete and post your question to the speaker(s). 4) Please, make sure you are in the right link and session. 1 Page Sponsored by: AB & BC Montney Technical Session Thursday, February 20th, 2020 801 Seventh +15 – 667 7 Street SW AGENDA 08:00 – 08:25 Registration, Networking and Breakfast 08:25 – 08:30 Welcome: Al Kassam and Dan Allan Montney Play Update Moderator: Karen Spencer, University of Calgary Moderator Bio: Ms. Spencer is an experienced oil and gas Professional Engineer with a Master’s Degree in Public Policy. Her unique background includes business and financial knowledge, strong technical experience, and a policy and regulatory focus. -
Forum's Value Proposition Copper-Cobalt-Uranium
JANICE LAKE SEDIMENTARY COPPER PROJECT, SASKATCHEWAN A RIO TINTO CANADA / FORUM ENERGY METALS EXPLORATION PROJECT Exploring for Energy Metals in North America May 11, 2019 www.forumenergymetals.com FEBRUARY 20, T2015SX.V: FMC Disclaimer The following presentation may contain forward-looking statements. Forward-looking statements address future events and conditions and therefore involve inherent risks and uncertainties. Actual results may differ materially from those currently anticipated in such statements. Forward-looking information is subject to known and unknown risks, uncertainties and other factors that may cause Forum’s actual results, level of activity, performance or achievements to be materially different from those expressed or implied by such forward-looking information. Such factors include, but are not limited to: uncertainties related to the historical resource estimates, the work expenditure commitments; the ability to raise sufficient capital to fund future exploration or development programs; changes in economic conditions or financial markets; changes in input prices; litigation; legislative, environmental and other judicial, regulatory, political and competitive developments; technological or operational difficulties or an inability to obtain permits required in connection with maintaining, or advancing projects its exploration projects and labour relations matters. All historical estimates were completed prior to the implementation of NI 43-101. A qualified person has not completed sufficient work to classify the historic estimates current mineral resources, and is not treating the historic estimates as current mineral resources. Hence, they should not be relied upon. Technical information has been prepared in accordance with the Canadian regulatory requirements set out in NI 43-101, and reviewed by Richard Mazur, P. -
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. -
Controls on Organic-Rich Mudstone Deposition: the Devonian Duvernay Formation, Alberta, Canada
Controls on organic-rich mudstone deposition: The Devonian Duvernay Formation, Alberta, Canada by Levi J. Knapp A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science Department of Earth and Atmospheric Sciences University of Alberta © Levi J. Knapp, 2016 Abstract: The Upper Devonian Duvernay Formation of Western Canada is a prolific source rock that in recent years has become an exploration target for shale gas and liquids. Development of the Duvernay Formation has demonstrated the importance of robust models for rock properties such as porosity, permeability, organic richness, and fracturability. Depositional processes and conditions govern the character and distribution of mudstone lithofacies, which are directly linked to variations in rock properties. The depositional and sequence stratigraphic models presented here are based on a detailed sedimentology and stratigraphy study. Twelve lithofacies were characterized based on lithology, sedimentary and biogenic structures, fossil type and abundance, and type and abundance of cement. Significant variation exists between organic-rich lithofacies, indicating that organic-rich mudstones were deposited in variably energetic and oxygenated environments, rather than within persistently anoxic, stagnant bottom waters. Correlation of core descriptions to a network of 759 wells with wireline logs led to the creation of a basin-scale sequence stratigraphic framework with 3 third order sequences. The sequence stratigraphic model shows a strong sea level and basin morphology control on basinal lithofacies. Transgression, and subsequent highstand normal regression in sequence 1 (oldest) resulted in significant platform construction in the northeast side of the basin. Sediments become consistently finer-grained and organic-rich away from the platform. -
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 …………………….……………..……. -
Sedimentology and Ichnology of Upper Montney Formation Tight Gas Reservoir, Northeastern British Columbia, Western Canada Sedimentary Basin
International Journal of Geosciences, 2016, 7, 1357-1411 http://www.scirp.org/journal/ijg ISSN Online: 2156-8367 ISSN Print: 2156-8359 Sedimentology and Ichnology of Upper Montney Formation Tight Gas Reservoir, Northeastern British Columbia, Western Canada Sedimentary Basin Edwin I. Egbobawaye Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Canada How to cite this paper: Egbobawaye, E.I. Abstract (2016) Sedimentology and Ichnology of Upper Montney Formation Tight Gas Re- Several decades of conventional oil and gas production in Western Canada Sedi- servoir, Northeastern British Columbia, mentary Basin (WCSB) have resulted in maturity of the basin, and attention is shift- Western Canada Sedimentary Basin. Inter- ing to alternative hydrocarbon reservoir system, such as tight gas reservoir of the national Journal of Geosciences, 7, 1357- 1411. Montney Formation, which consists of siltstone with subordinate interlaminated http://dx.doi.org/10.4236/ijg.2016.712099 very fine-grained sandstone. The Montney Formation resource play is one of Cana- da’s prime unconventional hydrocarbon reservoir, with reserve estimate in British Received: January 19, 2016 Columbia (Natural Gas reserve = 271 TCF), Liquefied Natural Gas (LNG = 12,647 Accepted: December 23, 2016 Published: December 28, 2016 million barrels), and oil reserve (29 million barrels). Based on sedimentological and ichnological criteria, five lithofacies associations were identified in the study interval: Copyright © 2016 by author and Lithofacies F-1 (organic rich, wavy to parallel laminated, black colored siltstone); Li- Scientific Research Publishing Inc. thofacies F-2 (very fine-grained sandstone interbedded with siltstone); Lithofacies This work is licensed under the Creative Commons Attribution International F-3A (bioturbated silty-sandstone attributed to the Skolithos ichnofacies); Lithofacies License (CC BY 4.0). -
Based on Superb Service to the Geoscience Profession and Academic Community, Particularly In
June 30, 2021 PRESS RELEASE For Immediate Release Saskatchewan Geoscientists, Donald Kent, P. Geo., P.Eng., FGC, FEC receives 2021 Canadian Professional Geoscientist Award Vancouver — Geoscientists Canada is pleased to announce the recipient of the 2021 Canadian Professional Geoscientist Award – Dr. Donald M. J. Kent, P.Geo., P.Eng., FGC, FEC, of Regina, SK The Canadian Professional Geoscientist Award recognizes the achievements of an individual who has made an outstanding contribution to the development and practice of professional geoscience and who has advanced public recognition of the profession in Canada in their capacity as a registered professional geoscientist. The award, which consists of a labradorite and marble sculpture made by a Canadian geoscientist artist, is given to a person in mid-to-late career. To be eligible for the award, a nominee must meet specified criteria, which include: a solid career as a professional geoscientist, an outstanding record of voluntary service to the community, and service to Geoscientists Canada or to one of the provincial or territorial professional associations that regulate geoscience practise in Canada. This year’s recipient of Geoscientists Canada’s highest honour, Dr. Donald Kent, is a distinguished award-winning geologist with long-standing research interests in the geology of carbonate hydrocarbon reservoir rocks. His contributions to understanding the petroleum geology of Canada, in particular the Williston Basin, provided much of the foundation upon which petroleum exploration in Saskatchewan was based. Dr. Kent holds a Ph.D. (1968) in Geology from the University of Alberta and a M.Sc. in Geology (1959) and B.Sc. (1957) in Geological Engineering from the University of Saskatchewan. -
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. -
Abstracts of Dmr Reports
- 222 - ABSTRACTS OF DMR REPORTS The following are abstracts of DMR reports by the Saskatchewan Geological Survey published or reprinted during the past year or scheduled to be released before 31 December, 1979: Beck, L.S. (1969; reprinted 1979): Uranium Deposits of the Athabasca Region; Sask., Dep. Min. Resour., Rep. 126, 139 p., 38 figs., 40 plates, 16 tables, 3 geol. maps. The Athabasca region is an important metallogenic largely pre-tectonic. In view of this, and because of the province of uranium and contains numerous epigenetic inherent structural differences between the two types of vein-type pitchblende deposits, some of which arc of geological environment, it is considered that the stable economic proportions, as well as many syngenetic occur blocks acted as relatively rigid units during the Hudsonian rences of uraninite in country rock and in pegmatite. This in contrast to the linear belts which were heavily faulted, report synthesizes existing geological information con mylonitized, and extensively granitized. Pitchblende cerning the region and presents the writer's own data bearing solutions were liberated during the final stages of collected over a four-year period as Resident Geologist at the Hudsonian granitization at about 1780 m.y. ago and Uranium City for the Saskatchewan Department of Mineral followed the crystallization of syngenetic uraninite in Resources and the results of subsequent work carried out at gneissic and granitic rocks transitionally. As the uranium the University of Leeds. The regional distribution, litho mineralization is related genetically to the Hudsonian logical and structural control, mineralogy, geochemistry, gra:iitization and mylonitization, the deposits are virtually and genesis of the uranium deposits are discussed and a restricted to the linear belts. -
Geochemical, Petrophysical and Geomechanical Properties Of
Geochemical, petrophysical and geomechanical properties of stratigraphic sequences in Horn River Shale, Middle and Upper Devonian, Northeastern British Columbia, Canada by TIAN DONG A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Earth and Atmospheric Sciences University of Alberta © Tian Dong, 2016 ABSTRACT The Middle and Upper Devonian Horn River Shale, comprising the Evie and Otter Park members and the Muskwa Formation, northeast British Columbia, Canada is recognized as a significant shale gas reservoir in the Western Canada Sedimentary Basin. However, many aspects of this shale formation have not been adequately studied, and the published geochemical, petrophysical and geomechanical data are limited. This work aims to document the controls of geochemical composition variation on petrophysical and geomechanical properties and the relationship of rock composition to lithofacies and stratigraphic sequences. A detailed core-based sedimentological and wireline log analysis was conducted by my colleague Dr. Korhan Ayranci as a parallel study, in order to classify lithofacies, interpret depositional environments and establish sequence stratigraphic framework across the basin. Major and trace elements concentrations, key trace element ratios and Corg-Fe-S relationships were used to understand the effect of sea level fluctuation on detrital flux, redox conditions, productivity and therefore organic carbon enrichment patterns. Detrital sediment flux indicated by the concentration of aluminum and titanium to the basin was found to be higher during transgressions than regressions. Redox conditions, exhibiting strong correlation to TOC content, were the primary controls on the organic carbon deposition. The bottom water conditions are more anoxic during transgressions than regressions. -
Facies Analysis and Ichnology of the Upper Montney Formation in Northeastern British Columbia
Facies Analysis and Ichnology of the Upper Montney Formation in Northeastern British Columbia A.E. Gegolick, University of Alberta, Edmonton, AB, [email protected] C.M. Furlong, University of Alberta, Edmonton, AB T.L. Playter, University of Alberta, Edmonton AB D.T. Prenoslo, University of Alberta, Edmonton, AB M.K. Gingras, University of Alberta, Edmonton, AB J.-P. Zonneveld, University of Alberta, Edmonton, AB Gegolick, A.E., Furlong, C.M., Playter, T.L., Prenoslo, D.T., Gingras, M.K. and Zonneveld, J.-P. (2016): Facies analysis and ichnology of the upper Montney Formation in northeastern British Columbia; in Geoscience BC Summary of Activities 2015, Geoscience BC, Report 2016-1, p. 111–116. Introduction tion are very heterogeneous. This refers to the several sedi- mentological and ichnological factors that result in highly The Lower Triassic Montney Formation is a world-class variable reservoir characteristics (e.g., Clarkson et al., unconventional hydrocarbon reservoir hosted primarily in 2012; Wood, 2013). Subtle changes in the rock fabric both low-permeability siltstone and to a lesser extent, very fine laterally and vertically result in the compartmentalization grained sandstone. To date, most published research has fo- of resources within zones of distinctly different porosity cused on conventional plays in the eastern part of the basin, and permeability values. Another controlling factor on res- such as the Montney Formation turbidite interval and ervoir properties is the occurrence of bioturbation. Biogen- shoreface clastic and bioclastic units proximal to the Trias- ic permeability is important to reservoir properties because sic subcrop edge (Davies et al., 1997; Moslow, 2000; it has the ability to either enhance or reduce permeability or Zonneveld et al., 2010a). -
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.