Devonian Gas Resources of the Western Canada Sedimentary Basin
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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. -
A Preliminary Assessment of the Native Fish Stocks of Jasper National Park
A Preliminary Assessment of the Native Fish Stocks of Jasper National Park David W. Mayhood Part 3 of a Fish Management Plan for Jasper National Park Freshwater Research Limited A Preliminary Assessment of the Native Fish Stocks of Jasper National Park David W. Mayhood FWR Freshwater Research Limited Calgary, Alberta Prepared for Canadian Parks Service Jasper National Park Jasper, Alberta Part 3 of a Fish Management Plan for Jasper National Park July 1992 Cover & Title Page. Alexander Bajkov’s drawings of bull trout from Jacques Lake, Jasper National Park (Bajkov 1927:334-335). Top: Bajkov’s Figure 2, captioned “Head of specimen of Salvelinus alpinus malma, [female], 500 mm. in length from Jaques [sic] Lake.” Bottom: Bajkov’s Figure 3, captioned “Head of specimen of Salvelinus alpinus malma, [male], 590 mm. in length, from Jaques [sic] Lake.” Although only sketches, Bajkov’s figures well illustrate the most characteristic features of this most characteristic Jasper native fish. These are: the terminal mouth cleft bisecting the anterior profile at its midpoint, the elongated head with tapered snout, flat skull, long lower jaw, and eyes placed high on the head (Cavender 1980:300-302; compare with Cavender’s Figure 3). The head structure of bull trout is well suited to an ambush-type predatory style, in which the charr rests on the bottom and watches for prey to pass over. ABSTRACT I conducted an extensive survey of published and unpublished documents to identify the native fish stocks of Jasper National Park, describe their original condition, determine if there is anything unusual or especially significant about them, assess their present condition, outline what is known of their biology and life history, and outline what measures should be taken to manage and protect them. -
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. -
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. -
Interview Summary
Interview Summary Interviewee: Ronnie Semansha Date: November 4, 2009 Location: Chateh Administration Office Interviewers: Kathrin Janssen, Adena Dinn “This [BC] is our traditional lands” -Ronnie Semansha Hunting and Trapping Ronnie hunts for moose in British Columbia (BC) near Kotcho Lake along the winter access road that spans from Rainbow Lake to Fort Nelson. He once shot a moose adjacent to Cabin Lake. He also uses the Sierra Yoyo Desan road and the winter access road that loops around Kotcho Lake for hunting. He takes this route once a week beginning on Friday afternoons when he is finished work. Ronnie also hunts in the area near Kwokullie Lake; he travels there via the winter access on the 31st baseline. Ronnie strictly hunts for moose in BC, and noted that there are hardly any caribou left. He explained that there used to be lots of caribou in BC but there has been a drop in recent times. Fishing Ronnie noted that there are pickerel in Kotcho Lake and explained that there are all different kinds of fish out there [BC]. Travel Routes Ronnie travels to BC using the winter access roads. He noted that there were two roads that he generally used, one from Rainbow Lake to Fort Nelson and one that cuts North to the Zama area (along the 31st baseline). When he does go out, other community members will often accompany him and everyone chips in a little for gas and supplies. However, he generally goes out for just one day and does not require supplies beyond fuel. Transcript 13 If he cannot travel to a certain area via the winter roads then Ronnie will often use a skidoo and the cutlines to access those areas. -
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 -
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. -
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. -
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. -
Faults and Associated Karst Collapse Suggest Conduits for Fluid Flow That Influence Hydraulic Fracturing-Induced Seismicity
Faults and associated karst collapse suggest conduits for fluid flow that influence hydraulic fracturing- induced seismicity Elwyn Gallowaya, Tyler Haucka, Hilary Corlettb, Dinu Pana˘ a, and Ryan Schultza,1 aAlberta Geological Survey, Alberta Energy Regulator, Edmonton, AB T8N 3A3, Canada; and bDepartment of Physical Sciences, MacEwan University, Edmonton, AB T5J 4S2, Canada Edited by Paul Segall, Stanford University, Stanford, CA, and approved August 21, 2018 (received for review May 1, 2018) During December 2011, a swarm of moderate-magnitude earth- bore [up to hundreds of meters (18–21)]. Furthermore, geo- quakes was induced by hydraulic fracturing (HF) near Cardston, mechanical modeling reveals that poroelastic changes from HF Alberta. Despite seismological associations linking these two processes, are transmitted only locally (20). These results are in direct the hydrological and tectonic mechanisms involved remain unclear. In contradiction to HF-related earthquakes that are located kilo- this study, we interpret a 3D reflection-seismic survey to delve into the meters away from the closest well bore (e.g., refs. 2, 6, 11, 22, and geological factors related to these earthquakes. First, we document a 23). Specific to the Cardston case, earthquakes (located on re- basement-rooted fault on which the earthquake rupture occurred that gional arrays) were observed within the uppermost crystalline ∼ – extends above the targeted reservoir. Second, at the reservoir’s strati- basement, 1.5 km deeper than the target upper Stettler Big SI Appendix graphic level, anomalous subcircular features are recognized along the Valley Reservoir zone ( ,Fig.S1); this observation is fault and are interpreted as resulting from fault-associated karst pro- further complicated by the fact that the fault slip response oc- ∼ – cesses. -
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. -
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.