15 Petrophysical Considerations in Evaluating the Montney
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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. -
CANADA's MOUNTAIN Rocky Mountain Goats
CANADA'S MOUNTAIN Rocky Mountain Goats CANADA'S MOUNTAIN PLAYGROUNDS BANFF • JASPER • WATERTON LAKES • YOHO KOOTENAY ° GLACIER • MOUNT REVELSTOKE The National Parks of Canada ANADA'S NATIONAL PARKS are areas The National Parks of Canada may, for C of outstanding beauty and interest that purposes of description, be grouped in three have been set apart by the Federal Govern main divisions—the scenic and recreational ment for public use. They were established parks in the mountains of Western Canada; the to maintain the primitive beauty of the land scenic, recreational, wild animals, and historic scape, to conserve the native wildlife of the parks of the Prairie Provinces; and the scenic, country, and to preserve sites of national his recreational, and historic parks of Eastern Can toric interest. As recreational areas they pro ada. In these pages will be found descriptions vide ideal surroundings for the enjoyment of of the national parks in the first group—areas outdoor life, and now rank among Canada's which lie within the great mountain regions outstanding tourist attractions. of Alberta and British Columbia. Canada's National Park system teas estab * * * lished in 1SS5, when a small area surrounding mineral hot springs at Banff in the Rocky This publication is compiled in co-operation Mountains was reserved as a public posses with the National Parks Branch, Department sion. From this beginning has been developed of Northern Affairs and National Resources. the great chain of national playgrounds note Additional information concerning these parks stretching across Canada from the Selkirk may be obtained from the Park Superintend Mountains in British Columbia to the Atlantic ents, or from the Canadian Government Travel Coast of Nova Scotia. -
1961 Climbers Outing in the Icefield Range of the St
the Mountaineer 1962 Entered as second-class matter, April 8, 1922, at Post Office in Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during March and December by THE MOUNTAINEERS, P. 0. Box 122, Seattle 11, Wash. Clubroom is at 523 Pike Street in Seattle. Subscription price is $3.00 per year. The Mountaineers To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanent form the history and traditions of this region; To preserve by the encouragement of protective legislation or otherwise the natural beauty of Northwest America; To make expeditions into these regions in fulfillment of the above purposes; To encourage a spirit of good fellowship among all lovers of outdoor Zif e. EDITORIAL STAFF Nancy Miller, Editor, Marjorie Wilson, Betty Manning, Winifred Coleman The Mountaineers OFFICERS AND TRUSTEES Robert N. Latz, President Peggy Lawton, Secretary Arthur Bratsberg, Vice-President Edward H. Murray, Treasurer A. L. Crittenden Frank Fickeisen Peggy Lawton John Klos William Marzolf Nancy Miller Morris Moen Roy A. Snider Ira Spring Leon Uziel E. A. Robinson (Ex-Officio) James Geniesse (Everett) J. D. Cockrell (Tacoma) James Pennington (Jr. Representative) OFFICERS AND TRUSTEES : TACOMA BRANCH Nels Bjarke, Chairman Wilma Shannon, Treasurer Harry Connor, Vice Chairman Miles Johnson John Freeman (Ex-Officio) (Jr. Representative) Jack Gallagher James Henriot Edith Goodman George Munday Helen Sohlberg, Secretary OFFICERS: EVERETT BRANCH Jim Geniesse, Chairman Dorothy Philipp, Secretary Ralph Mackey, Treasurer COPYRIGHT 1962 BY THE MOUNTAINEERS The Mountaineer Climbing Code· A climbing party of three is the minimum, unless adequate support is available who have knowledge that the climb is in progress. -
The Cambrian Explosion: a Big Bang in the Evolution of Animals
The Cambrian Explosion A Big Bang in the Evolution of Animals Very suddenly, and at about the same horizon the world over, life showed up in the rocks with a bang. For most of Earth’s early history, there simply was no fossil record. Only recently have we come to discover otherwise: Life is virtually as old as the planet itself, and even the most ancient sedimentary rocks have yielded fossilized remains of primitive forms of life. NILES ELDREDGE, LIFE PULSE, EPISODES FROM THE STORY OF THE FOSSIL RECORD The Cambrian Explosion: A Big Bang in the Evolution of Animals Our home planet coalesced into a sphere about four-and-a-half-billion years ago, acquired water and carbon about four billion years ago, and less than a billion years later, according to microscopic fossils, organic cells began to show up in that inert matter. Single-celled life had begun. Single cells dominated life on the planet for billions of years before multicellular animals appeared. Fossils from 635,000 million years ago reveal fats that today are only produced by sponges. These biomarkers may be the earliest evidence of multi-cellular animals. Soon after we can see the shadowy impressions of more complex fans and jellies and things with no names that show that animal life was in an experimental phase (called the Ediacran period). Then suddenly, in the relatively short span of about twenty million years (given the usual pace of geologic time), life exploded in a radiation of abundance and diversity that contained the body plans of almost all the animals we know today. -
British Columbia Geological Survey Geological Fieldwork 1990
GEOLOGY OF THE MOUNT BRUSSILOF MAGNESITE DEPOSIT, SOUTHEASTERN BRITISH COLUMBIA (825/12, 13) By George J. Simandl and Kirk D. Hancock KEYWOKLIS: Industrial minerals, rconomic geology. mag- nesitr. Cathedral Formation. Middle Cambrian. dolumitiz- tion, porosity. base metal association, deposit model. INTRODUCTION Magnesite (M&O,) is an induswial mineral that can bc converted into either caustic, fused or dead-burned magne- sia. Dead-burned magnesia is used mainly in the manufac- ture of refractory products; caustic magnesia is used in treatment of water, in animal feedstuffs, fertilizers. magne- sia cements, insulating boards and wood-pulp processing, in chemicals and pharmaceuticals and us a curing agent in rubber (Coope. 19X7). Magnesium metal is produced either from magnesite or from caustic mapnesia. In the short-term future. production of dead-burned mag- nesia is cxpectcd to remain constant. however, demand for caustic magnesia is increasing (Duncan, IYYO). With the increasing trend toward the use of high-perfomxmce “mag- carbon” refractories. future demand for fused magnesia looks promising. A number of magnesite deposits are known in British Columbia (Grzant, 19X7). the most important of these is the Mount Brussilof orebody. It is hosted by dolomites of the TECTONIC SETTING Middle Cambrian Cathedral Formation. The Mount Brussilof deposit is located in the Forekm3 rectonostratiEnlphic belt and within the “Kicking Horse HISTORY Rim”, as defined by Aitken (1971, 1989). It is situated east of a Cambrian bathymetric feature commonly referred to as The Mount Brussilof deposit was discovered during the Cathedral escarpment (Fritz. 1990: Aitken xnd regional mapping by the Geological Survey of Canada Mcllreath, 19X4, 1990). -
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). -
• Banff • Jasper • Kootenay • Yoho • Mount Revelstoke • Glacier • Waterton Lakes • National Parks • Fort St
• BANFF • JASPER • KOOTENAY • YOHO • MOUNT REVELSTOKE • GLACIER • WATERTON LAKES • NATIONAL PARKS • FORT ST. JAMES • BANFF PARK MUSEUM • CAVE AND BASIN • ROCKY MOUNTAIN HOUSE • BAR U RANCH • NATIONAL HISTORIC SITES Celebrating 100 years of this land and its stories e Ye f Jef 2007/2008 Également offert en français MAPS INSIDE! Welcome You are Visiting a National Treasure anadian national parks and Cnational historic sites are a country-wide system of significant natural areas, places, persons and events. These special locales are gateways to nature, adventure, discovery and to our past. They celebrate the beauty and infinite variety of our country and bear witness to our nation’s defining moments. Each national park is a sanctuary in And world heritage sites too! which nature is allowed to evolve in anff, Jasper, Kootenay and Yoho national parks, together its own way. Each national historic Bwith the provincial parks of Hamber, Mount Robson site tells a unique story, contributing and Mount Assiniboine, are recognized internationally as a a sense of time, identity, and place UNESCO World Heritage Site. The Canadian Rocky Mountain to our understanding of Canada as Parks World Heritage Site encompasses 20 585 km2–one of the a whole. largest protected areas in the world. Protected and preserved for all Waterton-Glacier International Peace Park, spanning the Canadians and for the world, Canada-U.S.A. boundary between Montana and Alberta, was Canada’s national parks and designated as a World Heritage Site because of its superlative national historic sites provide a mountain scenery, high topographic relief, glacial landforms, haven for plants and animals and and abundant diversity of wildlife and wildflowers. -
A Solution to Darwin's Dilemma: Differential Taphonomy of Ediacaran and Palaeozoic Non-Mineralised Discoidal Fossils
Provided by the author(s) and NUI Galway in accordance with publisher policies. Please cite the published version when available. Title A Solution to Darwin's Dilemma: Differential Taphonomy of Ediacaran and Palaeozoic Non-Mineralised Discoidal Fossils Author(s) MacGabhann, Breandán Anraoi Publication Date 2012-08-29 Item record http://hdl.handle.net/10379/3406 Downloaded 2021-09-26T20:57:04Z Some rights reserved. For more information, please see the item record link above. A Solution to Darwin’s Dilemma: Differential taphonomy of Palaeozoic and Ediacaran non- mineralised discoidal fossils Volume 1 of 2 Breandán Anraoi MacGabhann Supervisor: Dr. John Murray Earth and Ocean Sciences, School of Natural Sciences, NUI Galway August 2012 Differential taphonomy of Palaeozoic and Ediacaran non-mineralised fossils Table of Contents List of Figures ........................................................................................................... ix List of Tables ........................................................................................................... xxi Taxonomic Statement ........................................................................................... xxiii Acknowledgements ................................................................................................ xxv Abstract ................................................................................................................. xxix 1. Darwin’s Dilemma ............................................................................................... -
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 Mountain Life of Glen Boles Alpine Artistry the Mountain Life of Glen Boles
Alpine Artistry The Mountain Life of Glen Boles Alpine Artistry The Mountain Life of Glen Boles From anApisi test ratur aut quia que veriaectam volupta eperrum doluptat rem etur, sitatus enimi, el id quos imolor sit omnihiciae velliquas erovitius nossi rehendi cuptates niant lab intias moluptatessi ut est quunt, simi, conemoluptae voluptatiis dem dicietur? Nis sunt modit, occae sunt aliciis itatemperia quatiam facea consequid quam repudam ut lat. On pe volupta sanducid expe nesti blaborpore et, aute perovid ullaborit, quis eatibus tinctur? Tem quo omnim quo maion conesci atureriaeria nes es a susande pliquodipsum simporpora as et plabo. Namet reprendit eius evellat iasperr oriatur alignient.Ectaspis esercimus perum quod que cus autatusantur si dolupide il eosam, solupti dolorehende essi di repe conet aut anda int fugia voluptatium cullamus. Ut fuga. Nem nonsed ut odit dento etur, te omnihicae. Evenis estibus ducideris resto voluptatem cusae labores For further information regarding the Summit Series of mountaineering biographies, please contact the National Office of the Alpine Club of Canada. www.alpineclubofcanada.ca Nineteenth in the SUMMIT SERIES Biographies of people who have made a difference in Canadian mountaineering by Lynn Martel Alpine Artistry The Mountain Life of Glen Boles by Lynn Martel CANADIAN CATALOGUING IN PUBLICATIONS DATA Martel, Lynn. Alpine Artistry: The Mountain Life of Glen Boles Design by Suzan Chamney, Glacier Lily Productions. ISBN: 978-0-920330-53-1 © 2014, The Alpine Club of Canada All rights reserved. No portion of this book may be copied or reproduced without the permission of the author or the subject. The Alpine Club of Canada P.O. -
Pore-Scale Variability and Fluid Distributions in Montney Formation: New Insights from Three-Dimensional Reservoir Characterization and Modeling Sochi C
Pore-scale variability and fluid distributions in Montney Formation: New insights from three-dimensional reservoir characterization and modeling Sochi C. Iwuoha, Per K. Pedersen, and Christopher R. Clarkson Tight Oil Consortium, Department of Geoscience, University of Calgary, Alberta, Canada Fig.1 Montney Formation extent in Alberta and northeastern British Columbia Summary In the Triassic Montney Montney Formation in Alberta and British Columbia (Fig. 1 and 2), different fluids are produced (oil, gas condensate, dry gas). This study focuses on a Montney producing area in west central Alberta (Fig. 1) where thermal maturity and depth data are inconsistent with the production of different fluids. This evaluation reviews the potential control of pore size on fluid distributions in the study area. Our workflow utilizes well logs, core data and three-dimensional (3D) geological modeling techniques to map facies, petrophysical properties and pore size distribution in the study area. Our results show that gas and condensate producing areas have mean dominant pore throat sizes of 20 - 30nm with a wider range of pore size distribution (up to 55nm) occurring in the condensate producing area. The mainly oil producing area shows a lower mean dominant pore size of 10 - 20nm with a marked Fig. 2. Montney Formation and some overlying increase in siltstone and shale heterolithics eastwards. Although porosities in Cretaceous and Jurassic stratigraphy in the study area TVDSS GR RHOB the oil trend are relatively higher (mean ~4.5%) than those within the gas and 0 200 1.95 2.95 Kcardium Kcard_ss condensate producing areas (mean ~3% and 4% respectively), permeabilities Kkaskapau are lower in the oil trend (mean 0.27µD) compared to the gas (0.32µD) and condensate (0.48µD) producing areas. -
Commissioner Report-1913.Pdf
Photo by John Woodruff. Reflection of Mt. Run die in Vermilion Lakes, Banff, DEPARTMENT OF THE INTERIOR DOMINION OF CANADA. REPORT COMMISSIONER OF DOMINION PARKS FOlt TUB YEAR ENDING MAliCH 31 1913 I'ART V., ANNUAL REPORT, 1918 OTTAWA GOVERNMENT PRINTING BUREAU 1914 50406—1} DOMINION PARKS REPORT OF THE COMISSIONER OF DOMINION PARKS. DOMINION PARKS BRANCH, OTTAWA, September 30, 1913. W. W. CORY, Esq., C.M.G., Deputy Minister of the Interior. SIR,—I beg to submit my second annual report as Commissioner of Dominion Parks, covering the fiscal year 1912-13. Appended to it are reports from the Chief Superintendent of Dominion Parks and from the Superintendents of the various Parks. These reports show in detail the substantial progress made during the year in the matter of development work. My own report, therefore, is confined largely to a statement concerning the purposes served by National Parks and the useful develop ment work that such purposes suggest. CANADA'S PARKS. Extract from an address delivered at Ottawa. March 12, 1913, by His Royal Highness, the Duke of Connaught, before the Canadian Association for the Pre vention of Tuberculosis:— ' I feel that some apology is necessary for referring to the subject on which I now desire to touch, but the fact that this is the last onuortunity I shall have for public speaking before I go to England on leave must be my excuse. Also, the subject is allied with public health, which is one more reason for me to request your indulgence. ' I desire to refer shortly to the question of your Dominion Parks.