DOCSLIB.ORG

Summary of Field Activities in the Western Liard Basin, British Columbia Filippo Ferri, Margot Mcmechan, Tiffani Fraser, Kathryn Fiess, Leanne Pyle, Fabrice Cordey

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Summary of Field Activities in the Western Liard Basin, British Columbia Filippo Ferri, Margot Mcmechan, Tiffani Fraser, Kathryn Fiess, Leanne Pyle, Fabrice Cordey Summary of field activities in the western Liard Basin, British Columbia Filippo Ferri, Margot Mcmechan, Tiffani Fraser, Kathryn Fiess, Leanne Pyle, Fabrice Cordey To cite this version: Filippo Ferri, Margot Mcmechan, Tiffani Fraser, Kathryn Fiess, Leanne Pyle, et al.. Summary offield activities in the western Liard Basin, British Columbia. Geoscience Reports 2013, British Columbia Ministry of Natural Gas Development, pp.13-32, 2013, Geoscience Reports 2013. hal-03274965 HAL Id: hal-03274965 https://hal.archives-ouvertes.fr/hal-03274965 Submitted on 2 Jul 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. SUMMARY OF FIELD ACTIVITIES IN THE WESTERN LIARD BASIN, BRITISH COLUMBIA Filippo Ferri1, Margot McMechan2, Tiffani Fraser3, Kathryn Fiess4, Leanne Pyle5 and Fabrice Cordey6 ABSTRACT The second and final year of a regional bedrock mapping program within the Toad River map area (NTS 094N) was completed in 2012. The program will result in three– 100 000 scale maps of the northwest, northeast and southeast quadrants of 094N and with four 1:50 000 scale maps covering the southwest quadrant. Surface samples were also collected for Rock Eval™, reflective light thermal maturity and apatite fission-track analysis. Cuttings from several petroleum wells in the map area were also sampled for Rock Eval analysis and vitrinite reflectance. Composite sections of the Besa River Formation were measured in the southern Caribou Range and along the Alaska Highway, south of Stone Mountain. Approximately 170 m of the Besa River Formation were measured in three separate sections in the southern Caribou Range. Lithological, gamma-ray spectrometry and lithogeochemical data are similar to those observed in other sections of the formation, suggesting similar depositional conditions within the western Liard Basin. Changes in abundances of several trace elements, particularly, V, Mo, Ba and P, suggest variations in redox conditions during the deposition of the formation. Radiolarian and conodont fragments from the upper part of the section in the Caribou Range indicate a mid-Tournaisian age. Characteristics of the lower Besa River Formation observed along the Alaska Highway south of Stone Mountain are similar to the Evie member of the Horn River Formation. Ferri, F., McMechan, M., Fraser, T., Fiess, K., Pyle, L. and Cordey, F. (2013): Summary of field activities in the western Liard Basin, British Columbia; in Geoscience Reports 2013, British Columbia Ministry of Natural Gas Development, pages 13–31. 1Geoscience and Strategic Initiatives Branch, Oil and Gas Division, British Columbia Ministry of Natural Gas Development, Victoria, BC, [email protected] 2Geological Survey of Canada, Calgary, AB 3Yukon Geological Survey, Whitehorse, YT 4Northwest Territories Geoscience Office, Yellowknife, NWT 5VI Geosciences Services Ltd., Victoria, BC 6Université Claude Bernard Lyon 1, Lyon, France Key Words: Besa River Formation, Liard Basin, Horn River Basin, Toad River, regional mapping, shale gas, lithogeo- chemistry, gamma ray spectrometry, measured section, radiolarians, Caribou Range, British Columbia, Yukon, Northwest Territories. INTRODUCTION (GEM) Yukon Sedimentary Basins project. Examination of the Besa River Formation is in its third year and in 2012 The British Columbia Geoscience and Strategic Initia- was conducted as part of a multijurisdictional project be- tives Branch participated in two co-operative geosciences tween the governments of Yukon, Northwest Territories programs in the western Liard Basin during the summer of and British Columbia. This work was also supported by the 2012 (Fig. 1): 1) regional mapping within the Toad River GEM program through use of analytical laboratories at the map area (NTS 094N) and 2) examination of the Besa River Geological Survey of Canada (GSC). Formation in the western and northern Liard Basin. The re- Besa River stratigraphy exposed along the western gional mapping program is in its second year (McMechan margins of the Liard Basin contains equivalents to the Horn et al., 2012) and is part of the Geological Survey of Cana- River Formation, currently being developed for its shale da’s (GSC) ongoing Geomapping for Energy and Minerals gas potential in the eastern Horn River Basin (Fig. 2; Ferri BC Ministry of Natural Gas Development 13 o YT NWT 60 4 6 3 Maxhamish 7 Lk. 5 11 2 10 c-86-F 94P d-28-B 94O 94N Fort Nelson R. Liard R. 9 d-34-K d-69-k/94-O-2 1 77 8 Kotcho Lk. oad R. o T 59 Fort Nelson 97 94I 94K 94J 97 50 km 124o 122o Cretaceous-Tertiary Penn.-Permian Cambro-Ordovician 2010 2011 Upper Cretaceous Mississippian Cambrian study area study area Middle Cretaceous Devono-Missi. Upper Proterozoic 2012 Besa River Fm Triassic Ordovician-Devonian Middle Proterozoic study areas Regional Mapping Slave Point Edge Program Liard Basin (tick on basin side) 9 Petroleum well cuttings sampled for Rock Eval Horn River Basin conventional analysis. See Table 1 for gas field gas fields details. Apache Corp. Ltd. Figure 1 discovery wells Figure 1. Regional geological map of northern British Columbia showing the location of the regional mapping project in the Toad River map area (094N) and stratigraphic sections of the Besa River Formation measured in the southern Caribou Range and along the Alaska High- way, southeast of Toad River. Geological database from Massey et al. (2005). The edge of Horn River Basin follows the Slave Point edge as defined by Petrel Robertson Consulting Ltd. (2003). Well locations refer to data in Table 1. et al., 2011, 2012). The recent announcement by Apache carbonate and shale sequences of the Western Canada Sedi- Canada Ltd. of initial, average one-month production of mentary Basin (Fig. 2). Ferri et al. (2011, 2012) summarize 21.3 million cubic feet (mmcf; 6.03 × 105 m3) per day from the regional geological setting and stratigraphic framework a well within the central Liard Basin (d-34-K; Figure 1) of these rocks. underscores the potential for shale sequences in this area to hold significant potential. This well was drilled to a depth of 3800 m and laterally almost 900 m into the upper Besa TOAD RIVER MAPPING PROJECT (094N) River Formation. Apache Canada Ltd. estimates ultimate production of 17.9 billion cubic feet (5.06 × 108 m3) from This is the second year of a regional mapping program this well and suggests a net resource of 48 trillion cubic within the Toad River map area, spearheaded by the GSC. feet (1.36 × 1012 m3) on its 430 000 acre (174 021 Ha) land A summary of the geological setting, and stratigraphic and holdings (Apache Corporation Ltd., 2012; Macedo, 2012). structural framework, together with initial interpretations, can be found in McMechan et al. (2012). Rocks of the Besa River Formation represent western shale equivalents of Middle Devonian to Early Mississippian Two weeks were spent collecting field data within the Toad River map area (094N) from base localities in Fort 14 Geoscience Reports 2013 Liard Basin Horn River Basin Platform Permian Fantasque Formation Fantasque/Belloy Formation U Kindle Taylor Flat M Formation Fm Penn. L Mattson Mattson Kiskatinaw U Fm Fm Stoddart Gp Fm Golata Fm? Golata Fm? Golata Fm M Debolt Fm Debolt Formation Rundle Rundle Rundle Group Group Shunda Fm Group Shunda Formation (Prophet Fm) Pekisko Fm Pekisko Formation Mississippian Carboniferous L Banff Banff Formation Fm Banff Formation Exshaw Fm Exshaw Formation Exshaw Formation Fa Kotcho Fm Kotcho Formation Tetcho Fm Tetcho Formation Trout River Fm Trout River Formation Fort Fort Kakisa Fm Kakisa Formation Simpson Simpson Red Knife Upper Mbr Upper Fm Jean Marie Mbr Formation Formation Frasnian Fort Simpson Formation Muskwa Fm Muskwa Fm Muskwa Formation Besa River Formation Slave Point Fm Otter Watt Mtn Fm Devonian Park Otter Park Fm Fm Sulphur Point Fm Upper Keg Muskeg Fm Horn River Gp Horn River Gp Givetian Evie Fm Evie Fm River Fm Middle Dunedin Fm- Keg River Fm Lower Keg River Fm Ei Nahanni Fm Chinchaga Fm Chinchaga Fm L Em Stone Fm Sandstone Shale Carbonate Evaporite Chert Figure 2. Stratigraphic chart showing the relationship of the Besa River Formation to other shale units and carbonates within the Western Canada Sedimentary Basin. Figure 2 Nelson and at the small community of Liard River. A to- approximately 75 samples were collected for fossil iden- tal of 260 field stations were added during the 2012 field tification (unit age determination), thermal maturation via season, resulting in a total of nearly 1200 localities (Fig. reflective light microscopy, Rock Eval analysis and apatite 3). This includes BC Hydro coverage from the early 1980s fission track analysis for low-temperature thermal model- along the Liard River corridor and published and unpub- ling (i.e., burial and uplift history; Fig 3b). lished GSC data from the 1940s and late 1990s. In addition, BC Ministry of Natural Gas Development 15 o a) 60 BESA RIVER FORMATION This is the third year of a detailed stratigraphic and lithogeochemical examination of the Besa River Formation within the western Liard Basin (Ferri et al., 2011, 2012). In 2012, this project was carried out as part of a cooperative Liard River undertaking between the British Columbia Geoscience and Strategic Initiatives Branch, the Yukon Geological Survey Ft. Nelson and the Northwest Territories Geoscience Office. Because Besa River rock types occur in all three jurisdictions, an ap- Liard River River 97 proach using data from throughout this area would not only T oad River present a more complete picture of this emerging shale gas succession, it would also highlight the economic potential within all three regions.
Load more

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]
  • 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]
  • Pa 62-15.Pdf
    GEOLOGICAL SURVEY OF CANADA CANADA PAPER 62-15 MIDDLE DEVONIAN AND OLDER PALAEOZOIC FORMATIONS OF SOUTHERN DISTRICT OF MACKENZIE AND ADJACENT AREAS B y Helen R. Belyea and A. W. Norris DEPARTMENT OF MINES AND TECHNICAL SURVEYS CANADA CONTENTS Page Introduction. • . • . • • . • • . • • . • • 1 Ordovician and older(?) . • . • . • • • • • . • . • 1 Old Fort Island Formation........................... 2 Mirage Point Formation ...•...•..•. ,................ 2 Pre-Chinchaga beds . • • • . • • . • . • • • • . • . • • . • 3 Middle Devonian • . • . • . • • . • . • . • . • • . • 3 Chinchaga Formation ..•.•.••.•........•.•••••. • . • • • 3 Keg River Formation . • . • . • . • . • . • • • . 4 Muskeg Formation.................................. 5 Pine Point Formation................. .............. 5 Lonely Bay Formation • . • • • • . • . • • • • . • • 9 Sulphur Point Formation . • • . • . • . • . • . • . • • . • • . • . 10 Presqu 1ile Formation............................... 11 Watt Mountain Formation. • . • • • • . • . • . • • • • • . • . • . 12 Slave Point Formation . • • . • • • . • • . • • • • • • . • • • 12 Horn River Formation . • . • • . • • . • • • . • . • 14 References.............................................. 16 Appendix-logs of wells . • • • . • • • • • • . • . • • . • • • • • . • • . 19 Illustrations Figure 1. Formational nomenclature ••......•... .. .....•. Frontispiec e 2. Correla tion diagram from Pan American et al. A-1 Snake River c-28-D well to Imperial Triad Davidson C reek P-2 well .. ... ... •. .... ... .. in pocket 3. Correlation
    [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]
  • 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]
  • Alberta Basin. See Western Canada Foreland Basin. Alexander Terrane
    — ♦ — Index — ♦ — Alberta basin. See Western Canada foreland basin. Cardium Formation, 33, 35, 201, 202, 265, 302 Alexander terrane, 85 Cardium reservoir unit, 177, 178 Andean-type continental margin magmatic arc, Cascade basin, 273, 274 subduction along, 10 Cascade terrane, 85 Arctic Alaska plate, 376 Cassiar terrane, 85 Arctic National Wildlife Refuge (ANWR), 363 Charlie Lake Formation, 296 Arkoma basin, 436, 437, 443 Chinook Member, 36 Asmari reservoir, 331-332 Chugach terrane, 85, 116 Chungo Member, 33, 36 Bangestan/Qamchuqa reservoir, 332-333 Clearwater Formation, 27 Barrow arch, 375 Coastal belt terrane, 116, 118 Basal Colorado Sand reservoir unit, 170, 171 Coast plutonic complex, 11, 83 Bearpaw sandstones, 236 Colony Formation, 28 Beattie Peaks Formation, 18 Colorado Assemblage, 192,196-197, 199-201, 210-212, Belloy Formation, 297 224-226 Belly River Formation, 38, 117, 272 Colorado Group, 281-286, 300-303 Belly River reservoir unit, 181, 182 Colorado Group oils, 300 Belly River sandstones, 236 Colorado Shale, 284, 286 Belt Supergroup, 275 Crescent terrane, 116 Black Warrior basin, 431, 435, 436 Cummings Member, 24 Bluesky Formation, 22, 25 Cypress Hills/Hand Hills Assemblage, 192-193, 196-197, Boulder Batholith, 238 202-203 Bow Island Formation, 31, 32 Cypress Hills Formation, 42 Bowser basin, 85 Brazeau Formation, 39 Dakota sandstone, 414 Bridge River terrane, 85 Deep basin, Rock-Eval pyrolysis and TOC data, 283 Brookian sequence, 369-370, 370-374 Deformed belt, 84, 268-269 Dezful embayment. See Zagros foreland basin. Cache Creek
    [Show full text]
  • 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.
    [Show full text]
  • Liard Basin Hydrocarbon Project: Shale Gas Potential of Devonian-Carboniferous Strata in the Northwest Territories, Yukon and Northeastern British Columbia
    Liard Basin Hydrocarbon Project: Shale Gas Potential of Devonian-Carboniferous Strata in the Northwest Territories, Yukon and Northeastern British Columbia Kathryn M. Fiess, Northwest Territories Geoscience Office, Yellowknife, NT [email protected] and Filippo Ferri, Oil and Gas Division, BC Ministry of Energy, Mines and Natural Gas, Victoria, BC [email protected] and Tiffani L. Fraser, Yukon Geoscience Survey, Whitehorse, YT [email protected] and Leanne J. Pyle, VI Geoscience Services Ltd., Brentwood Bay, BC [email protected] and Jonathan Rocheleau, Northwest Territories Geoscience Office, Yellowknife, NT [email protected] Summary The Liard Basin Hydrocarbon Project was initiated in 2012 to examine the shale gas potential of Middle Devonian to Carboniferous strata based on integrated subsurface and outcrop-based field studies. The project is a collaboration of the Northwest Territories Geoscience Office (NTGO) with the Yukon Geological Survey, the British Columbia Ministry of Energy, Mines and Natural Gas and the Geological Survey of Canada. The primary objective of the project is to evaluate source rocks and refine stratigraphic correlation within the basinal succession of the Middle to Upper Devonian Besa River Formation and its Horn River “Formation” equivalents (Evie, Otter Park, and Muskwa members), as well as the Upper Devonian to Mississippian Exshaw Formation and Mississippian Golata Formation. The Liard Basin lies within three jurisdictions: the Northwest Territories (NT), Yukon (YK) and British Columbia (BC). In northeast BC it hosts several gas fields but remains largely underexplored in the NT and YK. During the initial field season, more than 500 m of strata were measured and described from three sections: 1) Golata Formation in the NT; 2) Besa River Formation in the YK; and 3) Besa River Formation in northeast BC.
    [Show full text]
  • Appendix E-1-1: Acid Rock Drainage and Metal Leaching Field Investigation
    AMEC Earth & Environmental a division of AMEC Americas Limited 2227 Douglas Road, Burnaby, BC Canada V5C 5A9 Tel +1 (604) 294-3811 Fax +1 (604) 294-4664 www.amec.com Acid Rock Drainage and Metal Leaching Field Investigation Enbridge Northern Gateway Project Submitted to: Northern Gateway Pipelines Inc. Calgary, AB Submitted by: AMEC Earth & Environmental, a division of AMEC Americas Limited Burnaby, BC October 2009 Revised February 16, 2010 AMEC File: EG09260.2300 Document Control No.: 1128-RG-20091022 Northern Gateway Pipelines Inc. Acid Rock Drainage and Metal Leaching Field Investigation October 2009 Revised February 16, 2010 TABLE OF CONTENTS Page LIST OF ABBREVIATIONS .......................................................................................................... v GLOSSARY ................................................................................................................................ vi EXECUTIVE SUMMARY .............................................................................................................. 1 1.0 INTRODUCTION .................................................................................................................. 2 1.1 Background ................................................................................................................. 2 1.2 Scope of Work ............................................................................................................. 2 2.0 INTRODUCTION TO ACID ROCK DRAINAGE ..................................................................
    [Show full text]
  • Alberta Table of Formations
    3D PGF v2 Model Fort Northern Central Southern Southern West- East- Northwest Northeast McMurray Grande ERATHEM / ERA Mountains Mountains Mountains Plains Central Central Plains Prairie Plains and Edmonton and Edmonton and Edmonton Edmonton Plains Edson Edmonton Plains Edmonton Edmonton Edmonton SYSTEM / PERIOD Foothills Jasper Foothills Foothills OF YEARS Banff SERIES / EPOCH Calgary AGE IN MILLIONS Blairmore Medicine STAGE / AGE Hat GC MC GC MC GC MC Laurentide Laurentide B Laurentide B B Laurentide Cordilleran Laurentide Cordilleran Laurentide Laurentide Cordilleran Cordilleran Laurentide BL BL QUATERNARY PLEISTOCENE Cordilleran EMPRESS EMPRESS EMPRESS EMPRESS EMPRESS PLIOCENE 2.6 5.3 DEL BONITA ARROWWOOD HAND HILLS WHITECOURT MOUNTAIN HALVERSON RIDGE PELICAN MOUNTAIN 7 NEOGENE MIOCENE 23 zone 1 OLIGOCENE CYPRESS HILLS OBED MOUNTAIN SWAN HILLS 34 EOCENE CENOZOIC 56 DALEHURST PALEOGENE PASKAPOOModel ZonesPASKAPOO PASKAPOO LACOMBE PALEOCENE HAYNES zonesPORCUPINE 2-3 HILLS PORCUPINE HILLS UPPER UPPER COALSPUR COALSPUR UPPER RAVENSCRAG UPPER 66 LOWER WILLOW CREEK WILLOW CK SCOLLARD SCOLLARD 01ENTRANCEsediment CONGLOMERATE above bedrock (surficial deposits) LOWER LOWER FRENCHMAN LOWER BATTLE BATTLE BATTLE WHITEMUD WHITEMUD MAASTRICHTIAN Bedrock topography CARBON ST. MARY RIVER ST. MARY RIVER HORSESHOE TOLMAN MORRIN UPPER UPPER EASTEND CANYON HORSESHOE 02 Paskapoo and Porcupine Hills formations HORSETHIEF CANYON 72 DRUMHELLER BLOOD RESERVE BLOOD RESERVE EDMONTON UPPER SAUNDERS SAUNDERS WAPITI / BRAZEAU STRATHMORE BRAZEAUScollard, Willow
    [Show full text]
  • Characterization and Evaluation of Deltaic Sandstone Reservoirs of the Dunvegan Formation, Kaybob South Arman Ghanbari, Steven M
    Characterization and Evaluation of Deltaic Sandstone Reservoirs of the Dunvegan Formation, Kaybob South Arman Ghanbari, Steven M. Werner, Lukas Sadownyk, Matthew Gonzalez, and Per Kent Pedersen Department of Geoscience, University of Calgary, Canada Summary Sandstones of the Cretaceous Dunvegan Formation within and around the Kaybob South Field are part of a legacy gas pool producing from a complex delta lobe. It is important to note that recently, oil production has also picked up in this area mainly with the implementation of horizontal wells. This presentation will investigate the complexities and variations of the Dunvegan from a geological perspective. Further, investigation will be undertaken on recent developments on a potential light oil play using horizontal drilling in the fine-grained deltaic sandstones of the Dunvegan. Introduction The Dunvegan Formation is a prolific gas producing unit in west-central Alberta. It was discovered in the 1950’s and has recently received attention for its oil production in horizontal wells within and near the Kaybob South (Figure 1). The area of focus in this study is the southwest of the Kaybob South region (Figure 1). This region also exhibits oil production on the peripheries of the pool where horizontal wells are located. The Dunvegan is stratigraphically trapped with deltaic sands acting as reservoir. The Dunvegan delta Figure 1. Adapted from Bhattacharya., 1994 – Kaybob gas pool is itself contains highly river marked by the yellow dot. The pool of study is within the red box where dominated deltas and a map of cumulative production is shown. Red production bubbles transgressive sheet sands indicate this is a gas dominated pool.
    [Show full text]
  • Shale Units of the Horn River Formation, Horn River Basin and Cordova Embayment, Northeastern British Columbia Sara Mcphail
    Shale units of the Horn River Formation, Horn River Basin and Cordova Embayment, Northeastern British Columbia Sara McPhail, Warren Walsh and Cassandra Lee British Columbia Ministry of Energy, Mines and Petroleum Resources Patrick A. Monahan, Monahan Petroleum Consulting/Penn West Energy Trust The Horn River Basin (HRB) and Cordova Embayment (CE) of northeastern British Columbia are bordered by the reef-fringed carbonate platforms of the Middle Devonian Upper Keg River, Sulphur Point, and Slave Point formations (Appendix A). Basinal shales laterally-equivalent to these carbonate units comprise the Evie, Otter Park, and Muskwa members of the Horn River Formation (Figure 1). These shales, particularly those of the Evie and Muskwa members that have high silica and organic contents are the target of a developing shale gas play. Figure 1: Middle and basal Upper Devonian units of the HRB and CE. basinal succession platform succession Fort Simpson Shale Muskwa Muskwa Upper Devonian Otter Park Slave Point Slave Pt/Sulphur Point basinal Middle Devonian equivalents Sulphur Point Evie Upper Keg River Lower Keg River Exploration activity for these shales in this lightly developed region has developed dramatically over the past two years (Adams et al, 2007). Total bonus paid for rights to the Horn River Shale exceeded $400 million in 2007. Experimental schemes, which allow an operator to hold well data confidential for 3 years, have been granted to several companies within the HRB and CE, and 48 wells have been licensed or drilled to test these targets since 2004 (Appendix A). Few results are available, but the recompletion of a vertical well in d-60-I/94-O-9 in the HRB resulted in a gas flow of 13 e3m3/, and EOG recently announced gas flow of 140 e3m3/d from their horizontal well in a-26-G/94-O-9.
    [Show full text]