Controls on Fluid Flow Systems in Northern Alberta As Related to MVT Mineralization: a Contribution to the Carbonate-Hosted Pb-Zn (MVT) Targeted Geoscience Initiative

Total Page:16

File Type:pdf, Size:1020Kb

Controls on Fluid Flow Systems in Northern Alberta As Related to MVT Mineralization: a Contribution to the Carbonate-Hosted Pb-Zn (MVT) Targeted Geoscience Initiative EUB/AGS Geo-Note 2002-21 Controls on Fluid Flow Systems in Northern Alberta as Related to MVT Mineralization: A Contribution to the Carbonate-Hosted Pb-Zn (MVT) Targeted Geoscience Initiative Alberta Energy and Utilities Board Alberta Geological Survey EUB/AGS Geo-Note 2002-21 Controls on Fluid Flow Systems in Northern Alberta as Related to MVT Mineralization: A Contribution to the Carbonate-Hosted Pb-Zn (MVT) Targeted Geoscience Initiative J.J. Adams* and D.R. Eccles Alberta Geological Survey September 2003 ©Her Majesty the Queen in Right of Alberta, 2003 The Alberta Geological Survey and its employees and contractors make no warranty, guarantee or representation, express or implied, or assume any legal liability regarding the correctness, accuracy, completeness, or reliability of this publication. Any digital data and software supplied with this publication are subject to the licence conditions. The data are supplied on the understanding that they are for the sole use of the licensee, and will not be redistributed in any form, in whole or in part, to third parties. Any references to proprietary software in the documentation, and/or any use of proprietary data formats in this release does not constitute endorsement by the Alberta Geological Survey of any manufacturer's product. When using information from this publication in other publications or presentations, due acknowledge- ment should be given to the Alberta Energy and Utilities Board/Alberta Geological Survey. The following reference format is recommended: Adams, J.J. and Eccles, D.R. (2003): Controls on fluid flow systems in northern Alberta as related to MVT mineralization: A contribution to the carbonate-hosted Pb-Zn (MVT) targeted geoscience initiative; Alberta Energy and Utilities Board, EUB/AGS Geo-Note 2002-21. Author contact information *J.J. Adams Formerly of Alberta Geological Survey [email protected] Published September 2003 by: Alberta Energy and Utilities Board Alberta Geological Survey 4th Floor, Twin Atria Building 4999 – 98th Avenue Edmonton, Alberta T6B 2X3 Tel: (780) 422-3767 (Information Sales) Fax: (780) 422-1918 E-mail: [email protected] Web site: www.ags.gov.ab.ca Cover Photo: Saline spring discharge on Lambert Creek, 3.2 km upstream from the confluence with Harper Creek. EUB/AGS Geo-Note 2002-21 (September 2003) • iii Contents Acknowledgements ....................................................................................................................................vi Abstract ....................................................................................................................................................vii 1 Introduction ..........................................................................................................................................1 2 Regional-scale Fluid Flow Systems in Northern Alberta..................................................................1 2.1 Alberta Basin Flow Systems............................................................................................................3 2.1.1 Present Day Regional Fluid Flow ........................................................................................3 2.1.2 Paleohydrogeology................................................................................................................4 3 Controls on Fluid Flow ........................................................................................................................6 3.1 Hydrostratigraphy ............................................................................................................................6 3.2 Permeability and Porosity ................................................................................................................8 3.3 Hydraulic Heterogeneities................................................................................................................9 3.3.1 Fluid Funnelling....................................................................................................................9 3.3.2 Permeability Enhancement....................................................................................................9 3.3.3 Heterogeneities in Northern Alberta ..................................................................................10 4 Controls on Mineralization ................................................................................................................10 4.1 Metals in Alberta Basement Rock ................................................................................................12 4.2 Formation Water Salinity ..............................................................................................................12 5 Potential Exploration Areas ..............................................................................................................15 6 References............................................................................................................................................15 Appendix A Surface Representation Grid Images for the Northeastern and Northwestern MVT Study Areas, Alberta ..............................................................................................22 Tables Table 1 Permeability and porosity data for northern Alberta ..................................................................8 Table A.1 List of formations with number of picks used in surface representation maps for the northeastern study area ........................................................................................25 Table A.2 List of formations with number of picks used in surface representation maps for the northwestern study area ......................................................................................26 Table A.3 Table of formations for northeastern Alberta with legend for the location of surface representation figures ................................................................................................................28 Table A.4 Table of formations for northwestern Alberta with legend for the location of surface representation figures ................................................................................................................32 Figures Figure 1 Basinal flow regimes: a) topography-driven flow due to tectonic rebound; b) thermo-haline convection during rifting; c) tectonically-driven flow during orogenic activity; d) compaction-driven flow; e) fault reactivation due to changes in the stress regime; and f) erosional-rebound flow ..............................................................2 Figure 2 Hydrostratigraphy of Alberta north of 56oN. Classification of each hydrostratigraphic unit was done based on Bachu and Undershultz (1992, 1993), Bachu (1997) and paleoreconstructions of the basin (Mossop and Shetsen, 1994) ............................................7 Figure 3 a) Areal extent of Devonian aquifers in the northern Alberta basin; and b) local highs in strata of northern Alberta. L = low, H = high, T = thin areas of the associated aquifer ..................................................................................................................11 Figure 4 Selected metal concentrations in Precambrian basement rocks in northern Alberta ............13 EUB/AGS Geo-Note 2002-21 (September 2003) • iv Figure 5 Present day formation water salinity in g/l TDS for a) Elk Point and b) Beaverhill Lake aquifer systems ......................................................................................14 Figure A.1 Isopach map showing the depth to the Devonian surface in northeastern Alberta…. ..........23 Figure A.2 Isopach map showing the depth to the Devonian surface in northwestern Alberta…..........24 Figure A.3 Surface representation maps for the top of the McMurray Formation ................................29 Figure A.4 Surface representation maps for the top of the Waterways Group…………………. ..........30 Figure A.5 Surface representation maps for the top of the Waterways Group using the AGS database……………………………………………………………………………………..31 Figure A.6 Surface representation maps for the top of the Bluesky Formation………………... ..........33 Figure A.7 Surface representation maps for the top of the Banff Formation……………………..........34 Figure A.8 Surface representation maps for the top of the Wabamun Group………………….. ..........35 Figure A.9 Surface representation maps for the top of the Winterburn Group. ..........…………………36 Figure A.10 Surface representation maps for the top of the Woodbend Group ........................................37 Figure A.11 Surface representation maps for the top of the Beaverhill Lake Group or top of the Waterways Group ..................................................................................................................38 Figure A.12 Surface representation maps for the top of the Slave Point Formation ............……………39 Figure A.13 Surface representation maps for the top of the Watt Mountain Formation ..........................40 Figure A.14 Surface representation maps for the top of the Sulphur Point Formation ............…………41 Figure A.15 Surface representation maps for the top of the Muskeg Formation......................................42 Figure A.16 Surface representation maps for the top of the Keg River Formation ..................................43 Figure A.17 Surface representation maps for the top of the Lower Keg River Formation ......................44 Figure A.18 Surface representation maps for the top of the Chinchaga Formation..................................45
Recommended publications
  • Northern Petroleum Virgo Technical Update NORTHERN PETROLEUM PLC
    Northern Petroleum Virgo Technical Update NORTHERN PETROLEUM PLC 23rd October 2014 Disclaimer These presentation materials (the "Presentation Materials") are being solely issued to and directed at persons having professional experience in matters relating to investments and who are investment professionals as specified in Article 19(5) of the Financial Services and Markets Act 2000 (Financial Promotion) Order 2005 (the "Financial Promotions Order") or to persons who are high net worth companies, unincorporated associations or high value trusts as specified in Article 49(2) of the Financial Promotions Order (“Exempt Persons”). The Presentation Materials are exempt from the general restriction on the communication of invitations or inducements to enter into investment activity on the basis that they are only being made to Exempt Persons and have therefore not been approved by an authorised person as would otherwise be required by section 21 of the Financial Services and Markets Act 2000 (“FSMA”). Any investment to which this document relates is available to (and any investment activity to which it relates will be engaged with) Exempt Persons. In consideration of receipt of the Presentation Materials each recipient warrants and represents that he or it is an Exempt Person. The Presentation Materials do not constitute or form any part of any offer or invitation to sell or issue or purchase or subscribe for any shares in Northern Petroleum PLC (“Northern Petroleum”) nor shall they or any part of them, or the fact of their distribution, form the basis of, or be relied on in connection with, any contract with Northern Petroleum relating to any securities.
    [Show full text]
  • Characterization of Geothermal Reservoir Units in Northwestern
    PROCEEDINGS, Thirty-Eighth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 11-13, 2013 SGP-TR-198 CHARACTERIZATION OF GEOTHERMAL RESERVOIR UNITS IN NORTHWESTERN ALBERTA BY 3D STRUCTURAL GEOLOGICAL MODELLING AND ROCK PROPERTY MAPPING BASED ON 2D SEISMIC AND WELL DATA Simon N. Weides1, Inga S. Moeck2, Douglas R. Schmitt2, Jacek A. Majorowicz2, Elahe P. Ardakani2 1 Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany 2 University of Alberta, 11322-89 Ave., Edmonton, AB, Canada e-mail: [email protected] the south-western part of the study area its temperature ABSTRACT is above 70 °C and the effective porosity is estimated with 10 % to 15 %. Foreland basins such as the Western Canada Sedimentary Basin (WCSB) host a variety of geoenergy Geothermal heat could play a role as energy source for resources. Often, the focus is on hydrocarbon resources district heating. In energy intensive in-situ oil sands but in times of discussions about climate change and extraction processes geothermal heat could be used for environmental aspects, additional green energy preheating of water for steam production. This would resources are under examination. This study explores lower the amount of natural gas used in oil sands Paleozoic formations in the north western WCSB with production and reduce climate gas emissions. regard to their usability as geothermal reservoirs. The study focuses on an area around Peace River in north – western Alberta. This research site covers an area of INTRODUCTION approx. 90 km * 70 km with a basin depth of 1.7 km to 2.4 km.
    [Show full text]
  • Helium in Northeastern British Columbia
    HELIUM IN NORTHEASTERN BRITISH COLUMBIA Elizabeth G. Johnson1 ABSTRACT Global demand for helium is increasing at a time when world reserves are in decline. The price of grade A helium has quadrupled in the past 12 years. Liquefied natural gas (LNG) processing can be used to capture helium as a value-added byproduct at concentrations as low as 0.04% by volume. The Slave Point, Jean Marie (Redknife) and Wabamun formations of northeastern British Columbia preferentially have helium associated with many of their natural gas pools. The mechanism for this accumulation appears to be flow in hydrothermal brines from helium-enriched basement granitic rocks along deeply seated faults. Separately, the Evie member of the Horn River Formation also has anomalous helium accumulation in its shale gas related to uranium decay in organic-rich shales. Johnson, E.G. (2012): Helium in northeastern British Columbia; in Geoscience Reports 2013, British Columbia Ministry of Natural Gas Development, pages 45–52. 1Geoscience and Strategic Initiatives Branch, British Columbia Ministry of Natural Gas Development, Victoria, British Columbia; [email protected] Key Words: Helium, LNG, Jean Marie, Slave Point, Wabamun, Evie, Horn River Formation INTRODUCTION optical fibre technology (8% of global use; Peterson and Madrid, 2012; Anonymous, 2012). Helium is a nonrenewable resource that has developed In recognition of its strategic value, the United States important strategic value. Helium (atomic number of 2) ex- 4 created the Federal Helium Reserve in the Bush Dome Res- ists primarily as the stable isotope, He, which is produced ervoir, Texas, in 1925. The primary source for the Federal on the earth through alpha decay of radioactive elements Helium Reserve is the world-class Hugoton Reservoir in such as uranium and thorium.
    [Show full text]
  • CO2 Storage in a Devonian Carbonate System, Fort Nelson British Columbia
    CO2 Storage in a Devonian Carbonate System, Fort Nelson British Columbia by Peter W. Crockford BSc., University of Victoria, 2008 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE in the School of Earth and Ocean Sciences Peter W. Crockford 2011 University of Victoria All rights reserved. This thesis may not be reproduced in whole or in part, by photocopy or other means, without the permission of the author. Library and Archives Bibliothèque et Canada Archives Canada Published Heritage Direction du Branch Patrimoine de l'édition 395 Wellington Street 395, rue Wellington Ottawa ON K1A 0N4 Ottawa ON K1A 0N4 Canada Canada Your file Votre référence ISBN: 978-0-494-88283-2 Our file Notre référence ISBN: 978-0-494-88283-2 NOTICE: AVIS: The author has granted a non- L'auteur a accordé une licence non exclusive exclusive license allowing Library and permettant à la Bibliothèque 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 télécommunication ou par l'Internet, prêter, telecommunication or on the Internet, distribuer et vendre des thèses partout dans le loan, distrbute and sell theses monde, à des fins commerciales ou autres, sur worldwide, for commercial or non- support microforme, papier, électronique et/ou commercial purposes, in microform, autres formats. paper, electronic and/or any other formats. The author retains copyright L'auteur conserve la propriété du droit d'auteur ownership and moral rights in this et des droits moraux qui protege cette thèse.
    [Show full text]
  • An Investigation of the Interrelationships Among
    AN INVESTIGATION OF THE INTERRELATIONSHIPS AMONG STREAMFLOW, LAKE LEVELS, CLIMATE AND LAND USE, WITH PARTICULAR REFERENCE TO THE BATTLE RIVER BASIN, ALBERTA A Thesis Submitted to the Faculty of Graduate Studies and Research in Partial Fulfilment of the Requirements For the Degree of Master of Science in the Department of Civil Engineering by Ross Herrington Saskatoon, Saskatchewan c 1980. R. Herrington ii The author has agreed that the Library, University of Ssskatchewan, may make this thesis freely available for inspection. Moreover, the author has agreed that permission be granted by the professor or professors who supervised the thesis work recorded herein or, in their absence, by the Head of the Department or the Dean of the College in which the thesis work was done. It is understood that due recognition will be given to the author of this thesis and to the University of Saskatchewan in any use of the material in this thesiso Copying or publication or any other use of the thesis for financial gain without approval by the University of Saskatchewan and the author's written permission is prohibited. Requests for permission to copy or to make any other use of material in this thesis in whole or in part should be addressed to: Head of the Department of Civil Engineering Uni ve:rsi ty of Saskatchewan SASKATOON, Canada. iii ABSTRACT Streamflow records exist for the Battle River near Ponoka, Alberta from 1913 to 1931 and from 1966 to the present. Analysis of these two periods has indicated that streamflow in the month of April has remained constant while mean flows in the other months have significantly decreased in the more recent period.
    [Show full text]
  • Keg River Oil and Gas Assessment Unit 52430102
    Keg River Oil and Gas Assessment Unit 52430102 135 130 125 120 115 65 # # 60 # ## ###### 5243 ############ ############ ###### # ########### # 5245 # ############ ## ######### # # ## # ## 55 Edmonton ÚÊ ÚÊ Calgary 50 Canada United States 0 250 500 KILOMETERS Keg River Oil and Gas Assessment Unit 52430102 Alberta Basin Geologic Province 5243 Other geologic province boundary USGS PROVINCES: Alberta Basin and Rocky Mountain Deformed Belt (5243 and 5245) GEOLOGIST: M.E. Henry TOTAL PETROLEUM SYSTEM: Keg River-Keg River (524301) ASSESSMENT UNIT: Keg River Oil and Gas (52430102) DESCRIPTION: This oil and gas assessment unit includes the northwestern part of the Alberta Basin and a small part of the east-central deformed belt. The area is generally bounded by the Tathlina High to the north and the Peace River Arch to the south. The eastern boundary is the estimated extent of potential reservoir rocks and the western boundary is the Keg River Gas assessment unit. SOURCE ROCKS: The principal source rocks are organic-rich, fine-grained rocks of the Middle Devonian Keg River Formation. MATURATION: The western half of this unit lies in the area where probable source rocks are expected to be mature with respect to liquid petroleum generation. MIGRATION: The distribution of oil and gas pools assigned to this unit in relation to the estimated distribution of mature source rocks indicates that long distance lateral migration is not required. RESERVOIR ROCKS: Virtually all reservoirs occur in dolomite, the majority of which developed in pinnacle reefs and many in patch reefs. TRAPS AND SEALS: The most common trap types are stratigraphic followed by structural and combination in the approximate proportion of 20 to five to one respectively.
    [Show full text]
  • Environmentally Significant Areas of Alberta Volumes 1, 2 and 3
    Environmentally Significant Areas of Alberta Volumes 1, 2 and 3 Prepared by: Sweetgrass Consultants Ltd. Calgary, AB for: Resource Data Division Alberta Environmental Protection Edmonton, Alberta March 1997 Environmentally Significant Areas of Alberta Volume 1 Prepared by: Sweetgrass Consultants Ltd. Calgary, AB for: Resource Data Division Alberta Environmental Protection Edmonton, Alberta March 1997 EXECUTIVE SUMMARY Large portions of native habitats have been converted to other uses. Surface mining, oil and gas exploration, forestry, agricultural, industrial and urban developments will continue to put pressure on the native species and habitats. Clearing and fragmentation of natural habitats has been cited as a major area of concern with respect to management of natural systems. While there has been much attention to managing and protecting endangered species, a consensus is emerging that only a more broad-based ecosystem and landscape approach to preserving biological diversity will prevent species from becoming endangered in the first place. Environmentally Significant Areas (ESAs) are important, useful and often sensitive features of the landscape. As an integral component of sustainable development strategies, they provide long-term benefits to our society by maintaining ecological processes and by providing useful products. The identification and management of ESAs is a valuable addition to the traditional socio-economic factors which have largely determined land use planning in the past. The first ESA study done in Alberta was in 1983 for the Calgary Regional Planning Commission region. Numerous ESA studies were subsequently conducted through the late 1980s and early 1990s. ESA studies of the Parkland, Grassland, Canadian Shield, Foothills and Boreal Forest Natural Regions are now all completed while the Rocky Mountain Natural Region has been only partially completed.
    [Show full text]
  • Watershed Resiliency and Restoration Program Maps
    VU32 VU33 VU44 VU36 V28A 947 U Muriel Lake UV 63 Westlock County VU M.D. of Bonnyville No. 87 18 U18 Westlock VU Smoky Lake County 28 M.D. of Greenview No. 16 VU40 V VU Woodlands County Whitecourt County of Barrhead No. 11 Thorhild County Smoky Lake Barrhead 32 St. Paul VU County of St. Paul No. 19 Frog Lake VU18 VU2 Redwater Elk Point Mayerthorpe Legal Grande Cache VU36 U38 VU43 V Bon Accord 28A Lac Ste. Anne County Sturgeon County UV 28 Gibbons Bruderheim VU22 Morinville VU Lamont County Edson Riv Eds er on R Lamont iver County of Two Hills No. 21 37 U15 I.D. No. 25 Willmore Wilderness Lac Ste. Anne VU V VU15 VU45 r Onoway e iv 28A S R UV 45 U m V n o o Chip Lake e k g Elk Island National Park of Canada y r R tu i S v e Mundare r r e Edson 22 St. Albert 41 v VU i U31 Spruce Grove VU R V Elk Island National Park of Canada 16A d Wabamun Lake 16A 16A 16A UV o VV 216 e UU UV VU L 17 c Parkland County Stony Plain Vegreville VU M VU14 Yellowhead County Edmonton Beaverhill Lake Strathcona County County of Vermilion River VU60 9 16 Vermilion VU Hinton County of Minburn No. 27 VU47 Tofield E r i Devon Beaumont Lloydminster t h 19 21 VU R VU i r v 16 e e U V r v i R y Calmar k o Leduc Beaver County m S Leduc County Drayton Valley VU40 VU39 R o c k y 17 Brazeau County U R V i Viking v e 2A r VU 40 VU Millet VU26 Pigeon Lake Camrose 13A 13 UV M U13 VU i V e 13A tt V e Elk River U R County of Wetaskiwin No.
    [Show full text]
  • Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area
    ERCB/AGS Special Report 093 Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area Stefan Bachu Maja Buschkuehle Kristine Haug Karsten Michael Alberta Geological Survey Alberta Energy and Utilities Board ©Her Majesty the Queen in Right of Alberta, 2008 ISBN 978-0-7785-6950-3 The Energy Resources Conservation Board/Alberta Geological Survey (ERCB/AGS) and its employees and contractors make no warranty, guarantee or representation, express or implied, or assume any legal liability regarding the correctness, accuracy, completeness or reliability of this publication. Any digital data and software supplied with this publication are subject to the licence conditions. The data are supplied on the understanding that they are for the sole use of the licensee, and will not be redistributed in any form, in whole or in part, to third parties. Any references to proprietary software in the documentation, and/or any use of proprietary data formats in this release, do not constitute endorsement by the ERCB/AGS of any manufacturer's product. If this product is an ERCB/AGS Special Report, the information is provided as received from the author and has not been edited for conformity to ERCB/AGS standards. When using information from this publication in other publications or presentations, due acknowledgment should be given to the ERCB/AGS. The following reference format is recommended: Bachu, S., Buschkuehle, M., Haug, K., Michael, K. (2008): Subsurface characterization of the Pembina-Wabamun acid-gas injection area; Energy Resources Conservation Board, ERCB/AGS Special Report 093, 60 p.
    [Show full text]
  • Geochemical Studies of Natural Gas, Part 1
    , ~ ( j ? j f GeoehelDieaI Studies of Natural Gas I PART m. INERT GASES IN WESTERN CANADIAN NATURAL GASES* ~ By BRIAN HITCHONt -j (This is the last of a Series of three Parts presented by the author tor publication in the Journal. Parts I I, and II appeared, in the Summer and Fall issues respectively.) ABSTRAGr 1 INTRODUcrION GEOCHEMISTRY AND ORIGIN OF In natural gases, the stratigra­ NITROGEN l phic and geographic variations in J T HIS paper is the third aud final Downloaded from http://onepetro.org/JCPT/article-pdf/2/04/165/2165406/petsoc-63-04-03.pdf by guest on 30 September 2021 1 the contents of both nitrogen and part of a series concerned with Before considering this subject heIiwn are of geochemical interest, further it is very important to con­ although only helium is of com­ the geochemistry of natural gas in 1 mercial importance. Nitrogen may Western Canada. It is a discussion sider the units in which the analy­ l originate from a great variety of of the inert gases nitrogen and he­ tical data are reported. Ideally, sources, including air, either orig­ lium. The first paper (1) dealt knowledge of the mass of the in­ J inally trapped in the sediments or '~ introduced dissolved in percolating with the hydrocarbons and the sec­ dividual components of natural groWldwaters, the denitrification of ond (2) with the acid gases. Due gases in the sedimentary basin is nitrogenous compounds or the de­ to their generally unreactive na­ desirable. From the reports of cay of certain radioactive minerals. ture, chemically, compared to hy­ Buckley and his co-workers (5) it In contrast, there exist radioac­ drocarbons or the acid gases, both may be surmised that the bulk of tive sources for all natural helium, nitrogen and helium are common­ the material is methane, with much and thus the problem of the migra­ lesser amounts .of other components.
    [Show full text]
  • 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.
    [Show full text]
  • Stratigraphic Trends in the Gething Formation
    Province of British Columbia ~’ MINERAL RESOURCES DIVISION Ministry of Energy, Mines and Geological Survey Branch Petroleum Resources STRATIGRAPHIC TRENDS IN THE GETHING FORMATION By A. Legun A Contribution to the Canada/British Columbia Mineral Development Agreement, 1985-1990 OPENFILE1990-33 Canadian Cataloging in Publication Data Legu”, Andrew s., 1949- Stratigraphic trends in the Gething Formation (Open file, ISSN 08353530 ; 1990-33) “A contribution to the Canada/British Columbia Mineral Devc,om”ent Am’eement, 19X5-1990.” VICTORIA BRITISH COLUMBIA CANADA 1. &thing Formation (B.C.) 2. Coal - Geology British Columbia - Peace River (Regional district) 3. Geology, March 1991 Stratigraphic. 4. Geology, Economic-British Columbia - l’eace River (Regional district) I. British Columbia. Geological Survey Branch. II. Canada/British Columbia Mineral Devclopmcnt Agreement. III. Title. IV. Series: yg3;f’ (British Columbia. Geological Survey Branch) ; QE187.443 1991 553.2’4’0971187 c91-092142-3 TABLE OF CONTENTS Page INTROD.UC’I’ION.. ..........................................1 General .........................................................1 Acknowledgments....................................... 1 GEOLOGY.. ......................................................3 Stratigraphic Trends.................................... 4 Chamberlain Member.. ........................4 Bullmoose Member ..............................7 Gaylard Member.. .................................7 Sourcesof Data.. ...................................8 SELECTED BIBLIOGRAPHY.. ...................9
    [Show full text]