In-Situ Stress Analysis of Southwest Saskatchewan
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Impact of Mineralogy and Diagenesis on Reservoir Quality of the Lower Cretaceous Upper Mannville Formation (Alberta, Canada)
Impact of Mineralogy and Diagenesis on Reservoir Quality of the Lower Cretaceous Upper Mannville Formation (Alberta, Canada). R. Deschamps, Eric Kohler, M. Gasparrini, O. Durand, T. Euzen, Fati Nader To cite this version: R. Deschamps, Eric Kohler, M. Gasparrini, O. Durand, T. Euzen, et al.. Impact of Mineralogy and Diagenesis on Reservoir Quality of the Lower Cretaceous Upper Mannville Formation (Alberta, Canada).. Oil & Gas Science and Technology - Revue d’IFP Energies nouvelles, Institut Français du Pétrole, 2012, 67 (1), pp.31-58. 10.2516/ogst/2011153. hal-00702841 HAL Id: hal-00702841 https://hal-ifp.archives-ouvertes.fr/hal-00702841 Submitted on 31 May 2012 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. ogst110074_Deschamps 22/02/12 14:54 Page 31 Oil & Gas Science and Technology – Rev. IFP Energies nouvelles, Vol. 67 (2012), No. 1, pp. 31-58 Copyright © 2012, IFP Energies nouvelles DOI: 10.2516/ogst/2011153 Dossier Diagenesis - Fluid-Rocks Interactions Diagenèse minérale - Équilibres fluides-roches Impact of Mineralogy and Diagenesis on Reservoir Quality of the Lower Cretaceous Upper Mannville Formation (Alberta, Canada) R. Deschamps1*, E. Kohler1, M. Gasparrini1, O. Durand2, T. Euzen3 and F. -
Saskatchewan Birding Trail Experience (Pdf)
askatchewan has a wealth of birdwatching opportunities ranging from the fall migration of waterfowl to the spring rush of songbirds and shorebirds. It is our hope that this Birding Trail Guide will help you find and enjoy the many birding Slocations in our province. Some of our Birding Trail sites offer you a chance to see endangered species such as Piping Plovers, Sage Grouse, Burrowing Owls, and even the Whooping Crane as it stops over in Saskatchewan during its spring and fall migrations. Saskatchewan is comprised of four distinct eco-zones, from rolling prairie to dense forest. Micro-environments are as varied as the bird-life, ranging from active sand dunes and badlands to marshes and swamps. Over 350 bird species can be found in the province. Southwestern Saskatchewan represents the core of the range of grassland birds like Baird's Sparrow and Sprague's Pipit. The mixed wood boreal forest in northern Saskatchewan supports some of the highest bird species diversity in North America, including Connecticut Warbler and Boreal Chickadee. More than 15 species of shorebirds nest in the province while others stop over briefly en-route to their breeding grounds in Arctic Canada. Chaplin Lake and the Quill Lakes are the two anchor bird watching sites in our province. These sites are conveniently located on Saskatchewan's two major highways, the Trans-Canada #1 and Yellowhead #16. Both are excellent birding areas! Oh! ....... don't forget, birdwatching in Saskatchewan is a year round activity. While migration provides a tremendous opportunity to see vast numbers of birds, winter birding offers you an incomparable opportunity to view many species of owls and woodpeckers and other Arctic residents such as Gyrfalcons, Snowy Owls and massive flocks of Snow Buntings. -
An Extra-Limital Population of Black-Tailed Prairie Dogs, Cynomys Ludovicianus, in Central Alberta
46 THE CANADIAN FIELD -N ATURALIST Vol. 126 An Extra-Limital Population of Black-tailed Prairie Dogs, Cynomys ludovicianus, in Central Alberta HELEN E. T REFRY 1 and GEOFFREY L. H OLROYD 2 1Environment Canada, 4999-98 Avenue, Edmonton, Alberta T6B 2X3 Canada; email: [email protected] 2Environment Canada, 4999-98 Avenue, Edmonton, Alberta T6B 2X3 Canada Trefry, Helen E., and Geoffrey L. Holroyd. 2012. An extra-limital population of Black-tailed Prairie Dogs, Cynomys ludovicianus, in central Alberta. Canadian Field-Naturalist 126(1): 4 6–49. An introduced population of Black-tailed Prairie Dogs, Cynomys ludovicianus, has persisted for the past 50 years east of Edmonton, Alberta, over 600 km northwest of the natural prairie range of the species. This colony has slowly expanded at this northern latitude within a transition ecotone between the Boreal Plains ecozone and the Prairies ecozone. Although this colony is derived from escaped animals, it is worth documenting, as it represents a significant disjunct range extension for the species and it is separated from the sylvatic plague ( Yersina pestis ) that threatens southern populations. The unique northern location of these Black-tailed Prairie Dogs makes them valuable for the study of adaptability and geographic variation, with implications for climate change impacts on the species, which is threatened in Canada. Key Words: Black-tailed Prairie Dog, Cynomys ludovicianus, extra-limital occurrence, Alberta. Black-tailed Prairie Dogs ( Cynomys ludovicianus ) Among the animals he displayed were three Black- occur from northern Mexico through the Great Plains tailed Prairie Dogs, a male and two females, originat - of the United States to southern Canada, where they ing from the Dixon ranch colony southeast of Val Marie are found only in Saskatchewan (Banfield 1974). -
Saskatchewan and Described in Attachment “1” to This Notice
TransCanada Keystone Pipeline GP Ltd. Keystone XL Pipeline Notice of Proposed Detailed Route Pursuant to Section 34(1)(b) (“Notice”) of the National Energy Board Act IN THE MATTER OF the National Energy Board Act, R.S.C. 1985, c. N-7 (“NEB Act”) and the regulations made thereunder; IN THE MATTER OF the Certificate of Public Convenience and Necessity OC-__ approving the general route of the Keystone XL Pipeline (“Pipeline”); AND IN THE MATTER OF an application by TransCanada Keystone Pipeline GP Ltd. (“Keystone”) respecting the determination and approval of the detailed route for the construction of a crude oil pipeline from Hardisty, Alberta to the international border near Monchy, Saskatchewan and described in Attachment “1” to this Notice.. If you anticipate that your lands may be adversely affected by the proposed detailed route of the Keystone Pipeline, you may oppose the proposed detailed route by filing a written statement of opposition with the National Energy Board (“Board”) within thirty (30) days following the publication of this notice. The written statement of opposition must set out the nature of your interest in those lands and the grounds for your opposition to the proposed detailed route. A copy of any such written statement of opposition must be sent to the following addresses: National Energy Board 444 – 7th Avenue SW Calgary, AB T2P 0X8 Attention: Anne-Marie Erickson, Secretary Toll Free Fax: (877) 288-8803 And to: TransCanada Keystone Pipeline GP Ltd. 101 – 6th Avenue SW Calgary, AB T2P 3P4 Attention: Ron Tourigny, Senior Land Representative – Keystone XL Pipeline Project Phone: (403) 920-7380 Fax: (403) 920-2325 Email: [email protected] Where a written statement is filed with the Board within the thirty (30) days of being served this notice, the Board shall forthwith order, subject to certain exceptions as noted below, that a public hearing be conducted within the area in which the lands to which the statement relates are situated with respect to any grounds of opposition set out in any such statement. -
Mesocyparis Rosanovii</Emphasis> Sp. Nov
ISSN 0031-0301, Paleontological Journal, 2006, Vol. 40, No. 3, pp. 328–338. © Pleiades Publishing, Inc., 2006. Original Russian Text © T.M. Kodrul, M.V. Tekleva, V.A. Krassilov, 2006, published in Paleontologicheskii Zhurnal, 2006, No. 3, pp. 93–102. A New Conifer Species, Mesocyparis rosanovii sp. nov. (Cupressaceae, Coniferales), and Transberingian Floristic Connections T. M. Kodrula, M. V. Teklevab, and V. A. Krassilovc aGeological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 109017 Russia e-mail: [email protected] bPaleontological Institute of Russian Academy of Sciences, ul. Profsoyuznaya 123, Moscow, 117997 Russia cInstitute of Evolution, University of Haifa, Mount Carmel 31905, Haifa, Israel Received October 25, 2005 Abstract—A new species, Mesocyparis rosanovii sp. nov. from the Lower Paleocene of the Amur Region, Rus- sia, is characterized by a combination of advanced and primitive features: mixed opposite-alternate branching of vegetative shoots, leafy microsporophylls, as well as a relatively high number of sporangia per microsporo- phyll and seeds per cone scale. The Late Cretaceous–Early Paleogene genus Mesocyparis McIver et Basinger, which obviously embraces a natural group of closely related species, was a significant component of the vege- tation in the middle and high latitudes of eastern Asia and western North America. The range of the genus tes- tifies to terrestrial Transberingian connections between the continents during the Cretaceous warming phases. DOI: 10.1134/S0031030106030142 Key words: conifers, Cupressaceae, Paleocene, Amur Region, Beringia, phytogeography. INTRODUCTION from each other, which would have virtually excluded the possibility of migration. The problem of floristic exchanges between eastern In this context, phytogeographic relations between Asia and western regions of North America has long Asia and North America should be revised using mod- attracted the attention of phytogeographers. -
Mannville Group of Saskatchewan
Saskatchewan Report 223 Industry and Resources Saskatchewan Geological Survey Jura-Cretaceous Success Formation and Lower Cretaceous Mannville Group of Saskatchewan J.E. Christopher 2003 19 48 Printed under the authority of the Minister of Industry and Resources Although the Department of Industry and Resources has exercised all reasonable care in the compilation, interpretation, and production of this report, it is not possible to ensure total accuracy, and all persons who rely on the information contained herein do so at their own risk. The Department of Industry and Resources and the Government of Saskatchewan do not accept liability for any errors, omissions or inaccuracies that may be included in, or derived from, this report. Cover: Clearwater River Valley at Contact Rapids (1.5 km south of latitude 56º45'; latitude 109º30'), Saskatchewan. View towards the north. Scarp of Middle Devonian Methy dolomite at right. Dolomite underlies the Lower Cretaceous McMurray Formation outcrops recessed in the valley walls. Photo by J.E. Christopher. Additional copies of this digital report may be obtained by contacting: Saskatchewan Industry and Resources Publications 2101 Scarth Street, 3rd floor Regina, SK S4P 3V7 (306) 787-2528 FAX: (306) 787-2527 E-mail: [email protected] Recommended Citation: Christopher, J.E. (2003): Jura-Cretaceous Success Formation and Lower Cretaceous Mannville Group of Saskatchewan; Sask. Industry and Resources, Report 223, CD-ROM. Editors: C.F. Gilboy C.T. Harper D.F. Paterson RnD Technical Production: E.H. Nickel M.E. Opseth Production Editor: C.L. Brown Saskatchewan Industry and Resources ii Report 223 Foreword This report, the first on CD to be released by the Petroleum Geology Branch, describes the geology of the Success Formation and the Mannville Group wherever these units are present in Saskatchewan. -
Physical and Numerical Modeling of SAGD Under New Well Configurations
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2013-09-23 Physical and Numerical Modeling of SAGD Under New Well Configurations Tavallali, Mohammad Tavallali, M. (2013). Physical and Numerical Modeling of SAGD Under New Well Configurations (Unpublished doctoral thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/27348 http://hdl.handle.net/11023/1002 doctoral thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Physical and Numerical Modeling of SAGD Under New Well Configurations by Mohammad Tavallali A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY DEPARTMENT OF CHEMICAL & PETROLEUM ENGINEERING CALGARY, ALBERTA SEPTEMBER, 2013 © Mohammad Tavallali, 2013 ii ABSTRACT This research was aimed at investigating the effect of well configuration on SAGD performance and developing a methodology for optimizing the well configurations for different reservoir characteristics. The role of well configuration in determining the performance of SAGD operations was investigated with help of numerical and physical models. Since mid 1980’s, SAGD process feasibility has been field tested in many successful pilots and subsequently through several commercial projects in various bitumen and heavy oil reservoirs. Although SAGD has been demonstrated to be technically successful and economically viable, it still remains very energy intensive, extremely sensitive to geological and operational conditions, and an expensive oil recovery mechanism. -
TGI Strat Column 2009.Cdr
STRATIGRAPHIC CORRELATION CHART TGI II: Williston Basin Architecture and Hydrocarbon Potential in Eastern Saskatchewan and Western Manitoba EASTERN MANITOBA PERIOD MANITOBA SUBSURFACE SASKATCHEWAN OUTCROP ERA glacial drift glacial drift glacial drift Quaternary Wood Mountain Formation Peace Garden Peace Garden Member Tertiary Member Ravenscrag Formation CENOZOIC Formation Goodlands Member Formation Goodlands Member Turtle Mountain Turtle Mountain Turtle Frenchman Formation Whitemud Formation Boissevain Formation Boissevain Formation Eastend Formation Coulter Member Coulter Member Bearpaw Formation Odanah Member Belly River “marker” Odanah Member Belly River Formation “lower” Odanah Member Millwood Member Lea Park Formation Millwood Member MONTANA GROUP Pembina Member Pembina Member Pierre Shale Pierre Shale Milk River Formation Gammon Ferruginous Member Gammon Ferruginous Member Niobrara Formation Chalky Unit Boyne Member Boyne Member Boyne Calcareous Shale Unit Member Carlile Morden Member Carlile upper Formation Morden Member Formation Morden Member Carlile Formation Assiniboine Marco Calcarenite Assiniboine Member Member CRETACEOUS Second White Specks Laurier Limestone Beds Favel Favel Keld Keld Member Member Formation Formation Belle Fourche Formation Belle Fourche Member MESOZOIC COLORADO GROUP Belle Fourche Member upper Fish Scale Formation Fish Scale Zone upper Base of Fish Scale marker Base of Fish Scale marker Westgate Formation Westgate Member lower Westgate Member Newcastle Formation Newcastle Member lower Viking Sandstone -
From the Late Cretaceous (Campanian) Kanguk Formation of Axel Heiberg Island, Nunavut, Canada, and Its Ecological and Geographical Implications MATTHEW J
ARCTIC VOL. 67, NO. 1 (MARCH 2014) P. 1 – 9 A Hadrosaurid (Dinosauria: Ornithischia) from the Late Cretaceous (Campanian) Kanguk Formation of Axel Heiberg Island, Nunavut, Canada, and Its Ecological and Geographical Implications MATTHEW J. VAVREK,1 LEN V. HILLS2 and PHILIP J. CURRIE3 (Received 1 October 2012; accepted in revised form 30 May 2013) ABSTRACT. A hadrosaurid vertebra was recovered during a palynological survey of the Upper Cretaceous Kanguk Formation in the eastern Canadian Arctic. This vertebra represents the farthest north record of any non-avian dinosaur to date. Although highly abraded, the fossil nonetheless represents an interesting biogeographic data point. During the Campanian, when this vertebra was deposited, the eastern Canadian Arctic was likely isolated both from western North America by the Western Interior Seaway and from more southern regions of eastern North America by the Hudson Seaway. This fossil suggests that large-bodied hadrosaurid dinosaurs may have inhabited a large polar insular landmass during the Late Cretaceous, where they would have lived year-round, unable to migrate to more southern regions during winters. It is possible that the resident herbivorous dinosaurs could have fed on non-deciduous conifers, as well as other woody twigs and stems, during the long, dark winter months when most deciduous plant species had lost their leaves. Key words: Appalachia, Arctic, Campanian, dinosaur, Laramidia, palaeobiogeography RÉSUMÉ. La vertèbre d’un hadrosauridé a été retrouvée pendant l’étude palynologique de la formation Kanguk remontant au Crétacé supérieur, dans l’est de l’Arctique canadien. Il s’agit de la vertèbre appartenant à un dinosaure non avien qui a été recueillie la plus au nord jusqu’à maintenant. -
Grasslands Plan Your Visit National Park
Grasslands Plan Your Visit National Park Let our friendly and knowledgeable staff, at both Visitor Centres, help you plan your Grasslands experience and assist you in having a safe and unforgettable adventure! Visitor Centre Hours of Operation West Block Activities Experience the solitude of May 17 - October 14, Daily 9:00 am - 5:00 pm 2019 the wide-open plain as the East Block prairie wind ripples a sea May 17 - September 2, Daily 9:00 am - 7:00 pm September 3 - October 14, Daily 9:00 am - 5:00 pm of grasses beneath the clear blue sky. Two unique Frenchman Valley Campground Kiosk West Block geographic locations: May 17 - September 2, Daily 3:00 pm - 9:00 pm West Block - Discover Contact Us the varied landscapes of West Block Visitor Centre (in Val Marie) 306-298-2257, Toll Free: 1-877-345-2257 the Frenchman River Valley and observe some of Rock Creek Visitor Centre (in East Block, Rock Creek Campground) 306-476-2018 Canada's rarest wildlife. The park is always open. Fees apply. Please visit the East Block - Explore the website for details. breathtaking badlands and discover astonishing dinosaur fossils exposed in Visit our website: Join us on Facebook the eroding layers of earth. parkscanada.gc.ca/ facebook.com/grasslandsnp grasslands Follow us on Twitter ©parkscanada sk Plan your visit to Grasslands National Park. Other Parks Canada Events in Saskatchewan Every Saturday July & August July 20 Frontier Life Waskesiu Children's Festival Fort Walsh National Historic Site Prince Albert National Park July 6 August 24 Louis Riel Relay & Kidfest Symphony Under the Batoche National Historic Site Sky Festival Motherwell Homestead National Historic Site .. -
General Geology of Lower Cretaceous Heavy Oil
POOR IMAGE DUE TO ORIGINAL DOCUMENT QUALITY -JC.plt, 5 - ot/-oI General Geology of Lower Cretaceous Heavy • Oil Accumulations In Western Canada By L W. VIGRASS* (Heavy Oil Semillur, The Petrolell1n Society of C.l.~I., Calgary. llIay .5, 1.965) ABSTRACT The oil throughout the belt is asphaltic and contain.'3Downloaded from http://onepetro.org/jcpt/article-pdf/4/04/168/2165766/petsoc-65-04-01.pdf by guest on 01 October 2021 large amounts of sulphur. nitrogen and oxygen. Gra Lower Cretaceous sand reservoirs contain about 750 billion barrels of "lscous, heavy oil along a broad arcuate vities range from 6° to 18° API and viscosities from belt that extends from northwestern Alberta into west several hundred to several million centipoise at GO°F, central Saskatchewan_ The heavy on is pooled in the Studies of sulphur isotopes, trace metal content and Mannville Group and, in a gross sense. occurs in a marine continental transition facies. The accumulation at Peace high molecular weight compounds show a fundamen River is in a regional onlap feature. The accumulations in tal similarity between Athabasca, Bonn.yville und the Athabasca-Llo}'dminster region occur across the Lloydminster crude oils. crest and on the southwest flank of a regional anticlinal feature associated with the solution of salt from Middle The change in character of the oil with geographic Devonian beds. These re~ional features had already position and depth is not ' ...·ell documented, but oils formed by the end of Early Cretaceous time. from deeper reservoirs at the south end of the bell Chemical and physical I)rOperties of oils from differ are more paraffinic, have higher API gravities and ent accumulations show that they belong to a single oil s:,.,stem and suggest a common mode of origin. -
Saskatchewan Conference Prayer Cycle
July 2 September 10 Carnduff Alida TV Saskatoon: Grace Westminster RB The Faith Formation Network hopes that Clavet RB Grenfell TV congregations and individuals will use this Coteau Hills (Beechy, Birsay, Gull Lake: Knox CH prayer cycle as a way to connect with other Lucky Lake) PP Regina: Heritage WA pastoral charges and ministries by including July 9 Ituna: Lakeside GS them in our weekly thoughts and prayers. Colleston, Steep Creek TA September 17 Craik (Craik, Holdfast, Penzance) WA Your local care facilities Take note of when your own pastoral July 16 Saskatoon: Grosvenor Park RB charge or ministry is included and remem- Colonsay RB Hudson Bay Larger Parish ber on that day the many others who are Crossroads (Govan, Semans, (Hudson Bay, Prairie River) TA holding you in their prayers. Raymore) GS Indian Head: St. Andrew’s TV Saskatchewan Crystal Springs TA Kamsack: Westminister GS This prayer cycle begins a week after July 23 September 24 Thanksgiving this year and ends the week Conference Spiritual Care Educator, Humboldt (Brithdir, Humboldt) RB of Thanksgiving in 2017. St. Paul’s Hospital RB Kelliher: St. Paul GS Prayer Cycle Crossroads United (Maryfield, Kennedy (Kennedy, Langbank) TV Every Pastoral Charge and Special Ministry Wawota) TV Kerrobert PP in Saskatchewan Conference has been 2016—2017 Cut Knife PP October 1 listed once in this one year prayer cycle. Davidson-Girvin RB Missing and Murdered Indigenous Women Sponsored by July 30 Imperial RB The Saskatchewan Conference Delisle—Vanscoy RB KeLRose GS Eatonia-Mantario PP Kindersley: St. Paul’s PP Faith Formation Network Earl Grey WA October 8 Edgeley GS Kinistino TA August 6 Kipling TV Dundurn, Hanley RB Saskatoon: Knox RB Regina: Eastside WA Regina: Knox Metropolitan WA Esterhazy: St.