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Helium in Southwestern Saskatchewan: Accumulation and Geological Setting
Open File Report 2016-1 Helium in Southwestern Saskatchewan: Accumulation and Geological Setting Melinda M. Yurkowski 2016 (Revised 14 December 2016) Saskatchewan Geological Survey ii Open File Report 2016-1 Open File Report 2016-1 Helium in Southwestern Saskatchewan: Accumulation and Geological Setting Melinda M. Yurkowski 2016 (Revised 14 December 2016) Printed under the authority of the Minister of the Economy © 2016, Government of Saskatchewan Although the Saskatchewan Ministry of the Economy has exercised all reasonable care in the compilation, interpretation and production of this product, 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 Saskatchewan Ministry of the Economy and the Government of Saskatchewan do not accept liability for any errors, omissions or inaccuracies that may be included in, or derived from, this product. This product is available for viewing and download at: http://www.publications.gov.sk.ca/deplist.cfm?d=310&c=176 Information from this publication may be used if credit is given. It is recommended that reference to this publication be made in the following form: Yurkowski, M.M. (2016): Helium in southwestern Saskatchewan: accumulation and geological setting; Saskatchewan Ministry of the Economy, Saskatchewan Geological Survey, Open File Report 2016-1, 20p. and Microsoft® Excel® file. Saskatchewan Geological Survey ii Open File Report 2016-1 Contents Introduction and Study Area .......................................................................................................................................... -
Jurassic Shaunavon Formation (Lower Melita): Structure Contour
Natural Resources Ressources naturelles Manitoba Science, Technology, Canada Canada Energy and Mines 19 48 Petroleum O O 106 00’ 0 96 00’ 0 O O O O 0 0 0 104 98 0 55 30’ O O 55 30’ 102 0 100 0 East Paint Lake Park Reserve Lac La Ronge La Ronge 70 6 O O 55 0 55 0 Snow Lake 106 Manitoba Flin Flon Saskatchewan 65 Grass River Provincial Park 39 2 60 10 Narrow Hills O O 54 0 Clearwater Lake Provincial Park 54 0 6 106 55 The Pas Lake 50 Nipawin 55 Prince Albert Carrot River Wildcat Hill Winnipeg Poplar/Nanowin Rivers Park Reserve O O 53 0 53 0 60 45 Melfort Tisdale Hudson Bay 3 6 Greenwater Lake 40 6 10 Chitek Lake Park Reserve Birch Island Park Reserve Humboldt 9 Kelvington O 35 Swan River O 52 0 16 52 0 Wadena 2 Preeceville Lanigan Wynyard Fisher Bay Park Reserve 16 Watrous 30 Foam Lake 10 Canora Duck Mountain Provincial Park Kamsack Good Spirit Lake 16 35 Davidson 0 Hecla/Grindstone Provincial Park -100 6 25 Yorkton Roblin -100 11 Dauphin O O 51 0 51 0 0 16 Melville -200 Riding Mountain National Park -100 Langenburg 20 Fort Qu’Appelle 0 Russell 10 Lumsden -200 Gimli Buffalo Pound 11 -100 Esterhazy Indian Head 1 Pilot Butte Balgonie 1 -300 Regina Moose Jaw 1 100 16 1 8 Grenfell 15 200 59 Lac du Bonnet 6 -400 1 Minnedosa Neepawa 200 16 Selkirk Stonewall 0 Beausejour Moosomin 44 Kipling O O 50 0 -300 -200 Birds Hill Provincial Park 50 0 Rivers Portage la Prairie 1 15 39 -100 Winnipeg 10 1 -500 -300 Carberry -400 Moose Mountain Brandon 1 Weyburn Spruce Woods Provincial Park Ste. -
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. -
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 -
Reservoir Characterization and Modelling of Potash Mine Injection Wells in Saskatchewan
RESERVOIR CHARACTERIZATION AND MODELLING OF POTASH MINE INJECTION WELLS IN SASKATCHEWAN A Thesis Submitted to the College of Graduate and Postdoctoral Studies In Partial Fulfillment of the Requirements For the Degree of Master of Science In the Department of Civil, Geological and Environmental Engineering University of Saskatchewan Saskatoon By DAVID PHILLIPS Copyright David Phillips, December, 2018. All rights reserved PERMISSION TO USE In presenting this thesis/dissertation in partial fulfillment of the requirements for a Postgraduate degree from the University of Saskatchewan, I agree that the Libraries of this University may make it freely available for inspection. I further agree that permission for copying of this thesis/dissertation in any manner, in whole or in part, for scholarly purposes may be granted by the professor or professors who supervised my thesis/dissertation work or, in their absence, by the Head of the Department or the Dean of the College in which my thesis work was done. It is understood that any copying or publication or use of this thesis/dissertation or parts thereof for financial gain shall not be allowed without my written permission. It is also understood that due recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis/dissertation. Requests for permission to copy or to make other uses of materials in this thesis/dissertation in whole or part should be addressed to: Head of the Department of Civil, Geological and Environmental Engineering University of Saskatchewan 57 Campus Drive, Saskatoon, Saskatchewan, S7N 5A9, Canada OR Dean College of Graduate and Postdoctoral Studies University of Saskatchewan 116 Thorvaldson Building, 110 Science Place Saskatoon, Saskatchewan, S7N 5C9, Canada i ABSTRACT In the Saskatchewan potash mining industry vast quantities of brine wastewater are generated from potash processing and mine inflow water. -
Williston Basin Project (Targeted Geoscience Initiative II): Summary Report on Paleozoic Stratigraphy, Mapping and Hydrocarbon A
Williston Basin Project (Targeted Geoscience Initiative II): Summary report on Paleozoic stratigraphy, mapping and GP2008-2 hydrocarbon assessment, southwestern Manitoba By M.P.B. Nicolas and D. Barchyn GEOSCIENTIFIC PAPER Geoscientific Paper GP2008-2 Williston Basin Project (Targeted Geoscience Initiative II): Summary report on Paleozoic stratigraphy, mapping and hydrocarbon assessment, southwestern Manitoba by M.P.B. Nicolas and D. Barchyn Winnipeg, 2008, reprinted with minor revisions January, 2009 Science, Technology, Energy and Mines Mineral Resources Division Hon. Jim Rondeau John Fox Minister Assistant Deputy Minister John Clarkson Manitoba Geological Survey Deputy Minister E.C. Syme Director ©Queen’s Printer for Manitoba, 2008, reprinted with minor revisions, January 2009 Every possible effort is made to ensure the accuracy of the information contained in this report, but Manitoba Science, Technol- ogy, Energy and Mines does not assume any liability for errors that may occur. Source references are included in the report and users should verify critical information. Any digital data and software accompanying this publication 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 Manitoba Science, Technology, Energy and Mines of any manufacturer’s product. When using information from this publication in other publications or presentations, due acknowledgment should be given to the Manitoba Geological Survey. The following reference format is recommended: Nicolas, M.P.B, and Barchyn, D. -
Hydrogeologic Framework for the Madison and Minnelusa Aquifers in the Black Hills Area
Hydrogeologic Framework for the Madison and Minnelusa Aquifers in the Black Hills Area by Jonathan D.R.G. McKaskey A thesis submitted to the Graduate Division in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE IN GEOLOGICAL ENGINEERING SOUTH DAKOTA SCHOOL OF MINES AND TECHNOLOGY RAPID CITY, SOUTH DAKOTA 2013 Prepared by: _____________________________________ Jonathan D.R.G McKaskey, Degree Candidate Approved by: _____________________________________ Dr. Arden Davis, Major Professor _____________________________________ Dr. Jennifer Benning, Graduate Division Representative _____________________________________ Dr. Kurt Katzenstein, Committee Member _____________________________________ Dr. Andrew Long, Committee Member _____________________________________ Dr. Laurie Anderson, Head of Department of Geology and Geological Engineering _____________________________________ Dr. Douglas Wells, Dean of Graduate Education i Abstract More than 50 percent of the public drinking water systems and more than 90 percent of the population in South Dakota rely solely on groundwater. This dependence on groundwater raises important questions regarding the Madison and Minnelusa aquifers in and near the Black Hills of South Dakota, including groundwater availability, the effects of water use or drought, mixing of regional flow and local recharge, and the effects of capture zones of springs and wells on the groundwater-flow system. These questions are best addressed with a three-dimensional numerical groundwater-flow model that -
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. -
Assessment of the Potential Heat Stored in the Aquifers/Reservoirs Of
ASSESSMENT OF THE POTENTIAL HEAT STORED IN THE DEEP AQUIFERS OF THE WILLISTON BASIN FOR GEOTHERMAL ENERGY PRODUCTION A Thesis Submitted to the College of Graduate and Postdoctoral Studies in Partial Fulfillment of the Requirements for the Degree of Master of Science in the Department of Civil, Geological and Environmental Engineering University of Saskatchewan By Lotanna Somadina Ufondu Copyright Lotanna S. Ufondu, July, 2017. All rights reserved. PERMISSION TO USE STATEMENT AND DISCLAIMER In presenting this thesis/dissertation in partial fulfillment of the requirement for a Postgraduate degree from the University of Saskatchewan, I agree that the Libraries of this University may make it freely available for inspection. I further agree that permission for copying of this thesis/dissertation in any manner, in whole or in part, for scholarly purposes may be granted by the professor or professors who supervised my thesis/dissertation work or, in their absence, by the Head of the Department or the Dean of the College in which my thesis work was done. It is understood that any copying or publication or use of this thesis/dissertation or parts thereof for financial gain shall not be allowed without my written permission. It is also understood that due recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis/dissertation. Requests for permission to copy or to make other uses of materials in this thesis/dissertation in whole or part should be addressed to: Head of the Department of Civil, Geological and Environmental Engineering 3B48.3 Engineering Building, 57 Campus Drive University of Saskatchewan Saskatoon, Saskatchewan S7N 5A9 Canada i ABSTRACT As the world shifts from fossil based energy generation towards renewable energy, it is important to consider the role geothermal energy can play in Saskatchewan. -
HERRERA-THESIS-2013.Pdf (12.72Mb)
A PETROLEUM SYSTEM STUDY OF THE CRATONIC WILLISTON BASIN IN NORTH DAKOTA, U.S.A.: THE ROLE OF THE LARAMIDE OROGENY A Thesis Presented to the Faculty of the Department of Earth and Atmospheric Sciences University of Houston -------------------------------------------- In Partial Fulfillment of the Requirements for the Degree Master of Science -------------------------------------------- By Henry Herrera August 2013 A PETROLEUM SYSTEM STUDY OF THE CRATONIC WILLISTON BASIN IN NORTH DAKOTA, U.S.A.: THE ROLE OF THE LARAMIDE OROGENY Henry Herrera APPROVED: Dr. Jolante Van Wijk, Chairman Dr. Guoquan Wang Dr. Constantin Sandu Dean, College of Natural Science and Mathematics ii DEDICATION To Jesus, my mom, dad, and sister, and all the people that believed in me. iii ACKNOWLEDGEMENTS I want to thank God because he is always with me. Thanks to my mother, father, and sister because they are always there for me. Thanks to Dr. Jolante Van Wijk because she supported me in good and bad moments during the thesis project, and did not let me quit. Thanks to Dr. Constantin Sandu and Dr. Wang for being part of my committee. I am thankful to Ismail Ahmad Abir and Kevin Schmidt for being patient helping me with my GIS problems. Thanks to Simon Echegu for his geochemical advice and friendship. Finally, thanks to the North Dakota Geological Survey (NDGS) for the provided information for the conclusion this thesis. iv A PETROLEUM SYSTEM STUDY OF THE CRATONIC WILLISTON BASIN IN NORTH DAKOTA, U.S.A.: THE ROLE OF THE LARAMIDE OROGENY An Abstract of a Thesis Presented to the Faculty of the Department of Earth and Atmospheric Sciences University of Houston -------------------------------------------- In Partial Fulfillment of the Requirements for the Degree Master of Science -------------------------------------------- By Henry Herrera August 2013 v ABSTRACT The Williston Basin is a Phanerozoic intracratonic basin located in the northern USA (North Dakota, South Dakota and Montana) and southern Canada (Manitoba and Saskatchewan). -
Structural Contour Map, Top of Deadwood Formation, Piedmont Quadrangle By
Structural Contour Map, Top of Deadwood Formation, Piedmont Quadrangle By (D A.L. Lisenbee, A.D. Davis, M.H. Price, and K.M. Grigg E A D M ) A E N 2012 S M E O D U A N E T M A T IN o 27'30" o R ) 103 30' 6 000m. 6 6 6 (TILFORD) 6 6 6 6 6 O 20 E. 21 22 R. 5 E. R. 6 E. 24 25 26 25' 27 28 29 103 22'30" (F o 44 15' o 0 4 510 8 44 15' 0 00 0 49 1 6 E 0 l 0 00 k 38 1 7 4 0 4 0 4 0 8 3 1 0 6 5 4 2 0 4200 31 0 8 49 000m. 0 00 N. 0 0 0 1 4 5 9 8 3 0 3 0 k 0 V 6 0 ree 0 46 T 0 C 0 00 0 2 4 49 0 3 0 00 0 H 2 3 1 5 0 0 0 3 9 0 0 2 51 4 0 2 00 3 0 35 0 0 00 4 0 5 0 0 3 V 4 0 00 4 0 9 4 3 3 3 6 0 7 00 0 0 Qal 0 3 3 2 3 3 0 1 5 4 0 420 0 0 0 0 9 0 0 4 0 7 0 4 4 0 T 0 3 0 0 8 4 48 4 0 0 0 99 7 6 49 0 0 0 00 0 0 4 4 5 4 2 0 0 3 0 0 0 10 0 12 7 8 9 2 0 10 48 11 OCd 0 4 6 4 0 99 4 7 0 0 A q u i f e r 0 2 A q u i f e r 5 0 4 0 4 2 0 6 0 0 Dalton Lake 0 4 49 1 00 0 2 0 7 0 0 36 Qal 4 00 4 50 700 0 R e c h a r g e 0 50 2 4 8 00 T 0 46 0 2 9 48 0 98 47 0 3 00 4900 3 9 0 0 3 F 0 0 50 4900 0 0 0 0 4 4 4898 A r e a 4 4 8 800 0 Spring 0 36 00 0 0 6 M 4 V 3800 0 0 0 47 5 00 Spring 3 18 16 800 5 17 15 14 0 13 Spring 0 15 0 4 5 0 49 0 00 4897 OCd 45 48 4 F 0 97 9 0 4 5 200 4 0 0 1 0 0 44 0 0 00 0 0 80 44 3 0 0 3 0 3 0 1 0 Sp 3 ring 0 3 2 0 3 0 3 0 0 4 0 0 3 OCd 80 0 4 M 5 0 0 0 0 450 4 4 48 Spring 0 96 0 12' 30" 4 12' 30" 0 1 4 0 0 8 9 0 0 4 4 48 0 9 0 96 0 M 22 23 24 19 20 21 22 Spring 3 6 0 3 0 4 3 7 7 4 3 8 0 2 0 00 0 4 0 0 45 4 9 0 0 8 3 4 0 0 0 0 0 0 0 0 0 0 0 0 51 4 8 0 0 0 48 00 95 4 48 00 00 5100 48 4895 0 0 46 4500 4 52 1 0 0 0 0 4 9 0 4 4 0 7 8 4 0 0 4 4 4 0 4 0 4 5 3 5 4 0 2 6 5 8 0 0 4 7 0 0 0 0 0 0 9 0 0 0 4 0 70 0 0 0 0 0 0 0 ( B L 5 48 A 27 0 26 25 30 29 28 27 94 C 0 0 K ) H 4 4 A O 8 4 48 0 0 4 W M 94 0 0 2 E 0 K 0 N 47 440 ) ( 00 0 0 0 6 4 4 00 90 5 0 43 0 0 0 0 7 0 4 Spring 49 00 4893 4600 0 4 0 7 4 0 4 0 48 0 Spring 0 93 4 4 8 9 8 4 4 0 8 0 0 0 0 0 5 1 0 0 4 2 0 0 34 35 36 31 32 33 34 0 0 4 4 k B e ox re e ld 4600 4 48 C e 6 92 r 0 0 0 0 4 0 50 4 5 0 0 60 0 0 47 48 s 0 92 e 0 t 6 T. -
The Letters F and T Refer to Figures Or Tables Respectively
INDEX The letters f and t refer to figures or tables respectively "A" Marker, 312f, 313f Amherstberg Formation, 664f, 728f, 733,736f, Ashville Formation, 368f, 397, 400f, 412, 416, Abitibi River, 680,683, 706 741f, 765, 796 685 Acadian Orogeny, 686, 725, 727, 727f, 728, Amica-Bear Rock Formation, 544 Asiak Thrust Belt, 60, 82f 767, 771, 807 Amisk lowlands, 604 Askin Group, 259f Active Formation, 128f, 132f, 133, 139, 140f, ammolite see aragonite Assiniboia valley system, 393 145 Amsden Group, 244 Assiniboine Member, 412, 418 Adam Creek, Ont., 693,705f Amundsen Basin, 60, 69, 70f Assiniboine River, 44, 609, 637 Adam Till, 690f, 691, 6911,693 Amundsen Gulf, 476, 477, 478 Athabasca, Alta., 17,18,20f, 387,442,551,552 Adanac Mines, 339 ancestral North America miogeocline, 259f Athabasca Basin, 70f, 494 Adel Mountains, 415 Ancient Innuitian Margin, 51 Athabasca mobile zone see Athabasca Adel Mountains Volcanics, 455 Ancient Wall Complex, 184 polymetamorphic terrane Adirondack Dome, 714, 765 Anderdon Formation, 736f Athabasca oil sands see also oil and gas fields, Adirondack Inlier, 711 Anderdon Member, 664f 19, 21, 22, 386, 392, 507, 553, 606, 607 Adirondack Mountains, 719, 729,743 Anderson Basin, 50f, 52f, 359f, 360, 374, 381, Athabasca Plain, 617f Aftonian Interglacial, 773 382, 398, 399, 400, 401, 417, 477f, 478 Athabasca polymetamorphic terrane, 70f, Aguathuna Formation, 735f, 738f, 743 Anderson Member, 765 71-72,73 Aida Formation, 84,104, 614 Anderson Plain, 38, 106, 116, 122, 146, 325, Athabasca River, 15, 20f, 35, 43, 273f, 287f, Aklak