Regional Correlation of the Beaverhill Lake Group in the Subsurface of Alberta, Townships 29 to 113 and Ranges 1W4 to 13W6 AER/AGS Open File Report 2014-05
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
Fever Master 2 August 11 2011
$100 Be Sure to Vote! Provincial Election Advance Polls open 9 a.m. to 8 p.m. Wednesday, Thursday, Friday, Saturday Election Day: Tuesday, May 5 9 a.m. to 8 p.m. Volume 16, Issue 17 Thursday, April 30, 2015 See Details on Pages 3, 6 & 7 At Lakeview Sports Center in Wabasca during last Saturday’s EXPO, NDP candidate Danielle Larivee (above left) makes a point, while (below) Wildrose can- didate Darryl Boisson shakes the hand of local fire- fighter Terri Lynn McLeod. Wabasca’s Triathlete Constable James Wood See more on Page 16 A Complete Line-Up of 2014 Ram 1500 SPORT New & Used CREW CAB Only 300 kms! #%#!# $ $ 00 #$%%# 49,000 %$ $##&$ $"" %$$# 00 "" " $" $ off! "" $ 18,000 Rugged & Ready PAGE 2 – Thursday, April 30, 2015 M.D. Expo attracts over 300 people Although the downturn nator, who was in charge of reach out to the community An indoor carnival with to Eagle Point Golf Course in the local economy proba- the trade-show, called the such as the Wabasca Fire children’s events was held to Freddie Gladue; bly affected the number of event a “great success, but it Department and Bigstone by the Outreach staff on the • An I-Pad from Fever exhibitors, the Land of Op- wouldn’t have been such Cree Nation Emergency jogging track above and Newspaper: Niki Gambler; portunity Expo held last Sat- without the amazing people Women’s Shelter. kept many children busy • A set of luggage pro- urday at Lakeview Sports here at the Lakeview Sports There was entertainment while their parents visited vided by Great Escapes was Center in Wabasca did at- Center, both the gym staff on the stage including the the vendors below. -
Natives Enter Mainstream Politics
Whoa! I said whoaaaaa... Dennis Samson of Hobbema twisted this critter sunshine and payoffs for the winners. down in 14 seconds flat, fast enough to grab fourth rounds are acknowledged as one of the place money. Samson and a whole mess of fin . -t in roe; ountry and the Indian rodeo circuit cowboys converged at Hobbema's Panee rodeo a ayytibr Afro -titors together for renewed grounds for the annual Spring Bust Out Rodeo. fr - ndshUonN I :t.'Ai .mpetition. The event got off wet and windy but wound up with 1Weft6 Te sty, Windspeaker Jat 2 7 rü Natives enter mainstream politics TERRY LUSTY, WiMSpeaker BY TERRY LUSTY Windspeaker Correspondent What a week it's been for Murial Stanley -Venne, Mike Cardinal and Willie Littlechild. The politicians have been nominated to represent their respective parties in separate elections. The first occurred June 11 when Muriel Stanley - Venne won the New Financial records Democratic nomination for the Yellowhead federal rid- ing currently held by PC kept Joe Clarke. from public In winning the NDP nom- ination for Yellowhead, BY DOROTHY SCHREIBER berships will be taken away Stanley -Venne will be out and LESLEY CROSSINGHAM "until we get rid of all the to unseat federal member troublemakers...there's no of Parliament Joe Clarke. law stating we have to put President of the Metis Stanley -Venne says she up with troublemakers." does not feel intimidated by Association Larry Des - Edson Local 44 president Clarke who is a meules has revoked mem- seasoned Sharon Johnstone and veteran when it comes to berships from individuals three of her members had requesting a look at the politics. -
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. -
Directory of Seniors' Centres in Alberta
DIRECTORY OF SENIORS’ CENTRES IN ALBERTA Directory of Seniors’ Centres in Alberta If you have any questions or require additional information, please call the Alberta Supports Contact Centre toll-free at 1-877-644-9992 or 780-644-9992 in Edmonton Directory Criteria Seniors’ centres included in the directory have met certain criteria. The centres must be not-for-profit and offer at least one on-going service or activity designed for seniors. Only those centres that submitted a completed questionnaire were considered for inclusion in the directory. Keeping Information Current The information contained in this document is subject to change. New seniors’ centres emerge and others move or disband. Updates will continue to be made to the website version of the directory at www.health.alberta.ca. To request a copy or to offer updates, please contact Alberta Health by mail, telephone or fax: Alberta Health Strategic Planning and Policy Development Division Policy Development and Community Partnerships Box 3100 Edmonton, Alberta T5J 4W3 Fax: (780) 422-8762 Telephone: Alberta Supports Contact Centre Toll-free: 1-877-644-9992 Edmonton and Area: (780) 644-9992 Acknowledgements Thank you to all the organizations that took the time to provide their information. Note The seniors’ centre street address is provided when available; however the postal code reflects the mailing address. Please contact the centre for complete mailing address if required. i © 2014 Government of Alberta Categories Used Services and programs described in the directory are listed in categories. The centre must offer at least one related service for the category to be listed. -
Petroleum System Modeling of the Western Canada Sedimentary Basin – Isopach Grid Files
Petroleum System Modeling of the Western Canada Sedimentary Basin – Isopach Grid Files By Debra K. Higley1, Mitchell E. Henry, and Laura N.R. Roberts Report Series 2005-1421 U.S. Department of the Interior U.S. Geological Survey 1 Inquiries about this publication should be addressed to: Debra K. Higley U.S. Geological Survey, MS 939, Box 25046 Denver Federal Center, Denver, CO 80225 Tel: 303-236-5791 Email: [email protected] 1 U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia 2005 For products and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS–the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Debra K. Higley, Mitchell Henry, and Laura N.R. Roberts, 2006, Petroleum System Modeling of the Western Canada Sedimentary Basin – Isopach Grid Files: U.S. Geological Survey Report Series 2005-1421, web publication and associated data files. Any use of trade, product, or firm names is for descriptive purposes only, and does not imply endorsement by the U.S. government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. 2 Contents Introduction …………………………………………………………….. 3 Data Processing Steps …………………………………………….……. 4 Acknowledgments ………………………………….………………..…. 5 Zmap-Format Grid Files ..………………………….………………..…. 5 References and Software Cited …………………….……………..……. -
Published Local Histories
ALBERTA HISTORIES Published Local Histories assembled by the Friends of Geographical Names Society as part of a Local History Mapping Project (in 1995) May 1999 ALBERTA LOCAL HISTORIES Alphabetical Listing of Local Histories by Book Title 100 Years Between the Rivers: A History of Glenwood, includes: Acme, Ardlebank, Bancroft, Berkeley, Hartley & Standoff — May Archibald, Helen Bircham, Davis, Delft, Gobert, Greenacres, Kia Ora, Leavitt, and Brenda Ferris, e , published by: Lilydale, Lorne, Selkirk, Simcoe, Sterlingville, Glenwood Historical Society [1984] FGN#587, Acres and Empires: A History of the Municipal District of CPL-F, PAA-T Rocky View No. 44 — Tracey Read , published by: includes: Glenwood, Hartley, Hillspring, Lone Municipal District of Rocky View No. 44 [1989] Rock, Mountain View, Wood, FGN#394, CPL-T, PAA-T 49ers [The], Stories of the Early Settlers — Margaret V. includes: Airdrie, Balzac, Beiseker, Bottrell, Bragg Green , published by: Thomasville Community Club Creek, Chestermere Lake, Cochrane, Conrich, [1967] FGN#225, CPL-F, PAA-T Crossfield, Dalemead, Dalroy, Delacour, Glenbow, includes: Kinella, Kinnaird, Thomasville, Indus, Irricana, Kathyrn, Keoma, Langdon, Madden, 50 Golden Years— Bonnyville, Alta — Bonnyville Mitford, Sampsontown, Shepard, Tribune , published by: Bonnyville Tribune [1957] Across the Smoky — Winnie Moore & Fran Moore, ed. , FGN#102, CPL-F, PAA-T published by: Debolt & District Pioneer Museum includes: Bonnyville, Moose Lake, Onion Lake, Society [1978] FGN#10, CPL-T, PAA-T 60 Years: Hilda’s Heritage, -
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. -
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. -
Cross-Section of Paleozoic Rocks of Western North Dakota
JolfN P. BLOEMLE N. D. Geological Survey NORTH DAKOTA GEOLOGICAL SURVEY WILSON M. LAIRD, State Geologist Miscel1aneous Series No. 34 CROSS-SECTION OF PALEOZOIC ROCKS OF WESTERN NORTH DAKOTA BY CLARENCE G. CARLSON Reprinted from Stratigraphic Cross Section of Paleozoic Rocks-Oklahoma to Saskatchewan, 1967: The American Association of Petroleum Geologists Cross Section Publication 5, p. 13-15, 1 Plate Grand Forks, North Dakota, 1967 NORTH DAKOTAI (Section E-F. Plate 5) C. G. CARLSON' Grand Forks, North Dakota INTRODUCTION which, in ascending order, are the Black Island, Icebox, The North Dakota segment of the cross section was and Roughlock. The Black Island generally consists of constructed with the base of the Spearfish Formation as clean quartzose sandstone, the Icebox of greenish-gray, noncalcareous shale, and the Roughlock of greenish-gray the datum. However, the Permian-Triassic boundary to brownish-gray, calcareous shale or siltstone. now is thought to be within redbeds of the Spearfish The Black Island and Icebox Formations can be Formation (Dow, 1964). If this interpretation is cor traced northward to Saskatchewan, but they have not rect, perhaps as much as 300 ft of Paleozoic rocks in been recognized as formations there and are included in well 3 and smaller thicknesses in wells I, 2, and 4-12 an undivided Winnipeg Formation. The Black Island are excluded from Plate 5. pinches out southwestward because of nondeposition Wells were selected which best illustrate the Paleozo along the Cedar Creek anticline, but the Icebox and ic section and its facies changes in the deeper part of Roughlock Formations, although not present on the the Williston basin. -
Duhamel: a Seismic Analysis of Differential Compaction in a Leduc Reef
The Duhamel reef Duhamel: A seismic analysis of differential compaction in a Leduc reef R.J. Brown, N.L. Anderson1, D.A. Cederwall2, Z. Sun, P.M. Manning3, and Q. Zhang ABSTRACT The Duhamel reef is an isolated Frasnian limestone bioherm of the Leduc Formation in south-central Alberta. Although Duhamel has a relatively small basal area (less than 12 km2), the reef rises some 275 m above the platform facies. The seismic data show what we interpret to be a raised peripheral reef rim, which appears to be elevated about 25 m relative to the interior of the reef. Raised rims are commonly considered to be diagenetic in origin, and attributed to differential compaction within reef complexes. Although late-stage accretionary growth about the periphery of the reef complex may have contributed to its development, we interpret the raised rim at Duhamel to be principally of secondary origin. This thesis is supported by the incorporated seismic and well-top data. The seismic data also suggest that the facies within the reef rim have a lower seismic velocity than the facies within the structurally lower reef interior, consistent with the observation that raised rims are generally more porous than the encircled and structurally lower lagoon and, therefore, constitute a preferred well-completion site. Optimal hydrocarbon recovery could be realized if all producing wells were drilled into the raised reef rim. Our data for Duhamel show that even relatively small reefs can exhibit raised rims and that these rims may be seismically visible, especially if one can incorporate multicomponent and/or 3-D data.