Iea Ghg Weyburn Co2 Monitoring & Storage Project Summary Report 2000-2004
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Preliminary Investigations of the Hudson Bay Area Coal Deposits
Preliminary Investigations of the Hudson Bay Area Coal Deposits J. Berenyi, A. Marsh, and R. Leray 1 Berenyi, J., Marsh, A., and Leray, R. (2009): Preliminary investigations of the Hudson Bay area coal deposits; in Summary of Investigations 2009, Volume 2, Saskatchewan Geological Survey, Sask. Ministry of Energy and Resources, Misc. Rep. 2009-4.2, Paper A-12, 14p. Abstract The discovery of anomalous thicknesses of coal in the Hudson Bay region of east-central Saskatchewan by Goldsource Mines Inc., in the spring of 2008, ignited an unprecedented staking rush for coal in the province. Subsequent drilling by the company has shown that these deposits are not only anomalous in thickness, but also in morphology and depositional environment. Unlike most other coal deposits in Saskatchewan, which are relatively thin (less than a few metres) and more regionally extensive, the Hudson Bay area coal deposits are more localized and have far greater thicknesses of up to 100 m (including partings). Since the initial discovery, the company has identified a total of 11 discrete coal deposits within its 51 942 ha Border Project area. In June of 2009, Saskatchewan Ministry of Energy and Resources staff commenced a study of the stratigraphy, sedimentology, and diagenetic history of the subsurface in and around these discoveries in an attempt to develop a geologic model for these types of deposits. Detailed stratigraphic logging, combined with geophysical well log interpretation, provided the basis for some preliminary interpretations. All of the significant intervals of coal occur within the Cantuar Formation of the Mannville Group. The Cantuar Formation is infilling paleo-topographic lows on the sub-Cantuar unconformity surface. -
Preliminary Report on Sedimentology and Stratigraphy of the Late Devonian Mixed Carbonate-Evaporite Succession of the Duperow Formation, Southeastern Saskatchewan
Preliminary Report on Sedimentology and Stratigraphy of the Late Devonian Mixed Carbonate-Evaporite Succession of the Duperow Formation, Southeastern Saskatchewan X.C. Cen 1 and O. Salad Hersi 1 Cen, X.C. and Salad Hersi, O. (2005): Preliminary report on sedimentology and stratigraphy of the Late Devonian mixed carbonate-evaporite succession of the Duperow Formation, southeastern Saskatchewan; in Summary of Investigations 2005, Volume 1, Saskatchewan Geological Survey, Sask. Industry Resources, Misc. Rep. 2005-4.1, CD-ROM, Paper A-9, 12p. Abstract The Duperow Formation of southeastern Saskatchewan is divided into four informal units (1 to 4). These units are defined by various lithofacies of laminated to thickly bedded bioclastic limestones, thinly to microbially laminated dolostone, laminated to nodular anhydrite, and rare halite deposits. Bioclasts in the limestone lithofacies include gastropods, bivalves, brachiopods, and stromatoporoids, and represent deposition within an open- to restricted- marine to lagoonal setting. The dolostone, anhydrite, and halite strata are interpreted as supratidal deposits. Limestone, dolostone, and anhydrite comprise the three prominent lithofacies and are preserved as “restricting- upward” rhythmites. The development of repetitive patterns of lithofacies is attributed to cycles of intermittent invasions of normal marine water which evolved to hypersaline brine by evaporative processes. The lateral continuity and regional significance of rhythmites of the Duperow Formation as exhibited by sedimentological, stratigraphic, and microfacies characteristics, and their impact on reservoir quality, are the focus of an on-going research project. Keywords: Duperow Formation, southeastern Saskatchewan, Late Devonian, carbonates, evaporites, rhythmic succession, shallow marine. 1. Introduction This study is focused on sedimentological and stratigraphic features of the Late Devonian Duperow Formation of southeastern Saskatchewan. -
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 -
RI7120100316.Pdf
..- "" .. ~. ------ TIGRAPHIC NAMES DAKOTA ") " ........ / \ ~ / / / --- \ \ / \ \ } ' ) " I / \ ) \ /' /" /''' , \ . ./ " "1 /' ,. ) ~ / "- ~ " \. " LEXICON OF STRATIGRAPHIC NAMES j ft OF NORTH DAKOTA i by Joanne Lerud REPORT OF INVESTIGATION NO. 71 NORTH DAKOTA GEOLOGICAL SURVEY Don L. Halvorson, State Geologist 1982 Printed by Kaye's Inc., Fargo, ND 58102 1982 ...:. CONTENTS Page INTRODUCTION 1 LEXICON . 2 REFERENCES 113 APPENDIX A--NAMED LIGNITE BEDS IN NORTH DAKOTA 115 APPENDIX B--PLEISTOCENE AND HOLOCENE STRATIGRAPHIC NAMES 129 SELECTED BIBLIOGRAPHY--PLEISTOCENE AND HOLOCENE STRATIGRAPHIC TERMINOLOGY . 137 ILLUSTRATIONS Plate 1. North Dakota Stratigraphic Column . (in pocket) INTRODUCTION This lexicon is a modified version of a master's thesis completed at the University of North Dakota entitled, "Lexicon of Bedrock Stratigraphic Names of North Dakota" by Joanne Van Ornum Groenewold (now Joanne V. Lerud). In the thesis she attempted to include all terms previously applied to these strata in North Dakota together with a history of the unit, age, area of extent, lithology, thickness, relationships to other units, characteristic fossils, econ 0mic significance, depositional environment, and references to type sections. An attempt to show accepted North Dakota usage was presented by a system of capitalization and underlining. The thesis was entirely a literature search with the information provided for each entry being an edited sum of available information for that term. The lexicons of geologic names of the United States by M. Grace Wilmarth (USGS Bulletin 896) and G. C. Keroher (USGS Bulletins 1200 and 1350) were used extensively for the historical summaries. South Dakota Geological Survey Bulletin 14, entitled, "A guide to the Stratigraphy of South Dakota," by Allen F. Agnew and Paul C. -
Evidence of the Potential for Mississippi Valley-Type Lead-Zinc
o eol gic g a a l b s o u t r i v n e a MGS y m Update on industrial mineral and stratigraphic investigations in Manitoba 1928 K. Lapenskie, Manitoba Geological Survey Evidence of the potential for Mississippi Gypsum resources in the Amaranth area, west High-purity silica sand of the Winnipeg Phanerozoic corelogging activities in Valley-type lead-zinc deposits in Manitoba shore Lake Manitoba Formation southwestern Manitoba 101°00'W Introduction Summary Introducon Legend Summary DEVONIAN In 2015, the MGS initiated an investigation into the gypsum resources of Manitoba (Lapenskie and Bamburak, 2015). The aim of this The Winnipeg Formation contains some of the purest silica sand deposits in North America. Historically, this silica sand has been Mississippi Valley-type (MVT) deposits consist of stratabound, SBZ The lower Paleozoic stratigraphic framework of southwestern Manitoba contains many inconsistencies (Lammers, 1988; Bezys and ORR DSR Souris River Formation project is to provide a comprehensive update on this commodity, which has been utilized for industrial purposes in Manitoba for over 100 quarried and processed in the province to produce glass. The MGS is re-examining this formation to determine the economic potential of carbonate-hosted assemblages of sphalerite, galena and iron Conley, 1998; Nicolas and Barchyn, 2008; Lapenskie and Nicolas, 2017) (Figure 1). Lateral variations in lithology, facies changes and DDB Dawson Bay Formation years (Bannatyne, 1959, 1977; Gunter, 1987). Economic deposits of gypsum occur in the evaporitic Upper Amaranth Member of the the silica sand for a variety of applications, including as a very high quality proppant for fracking. -
2004 Mesozoic Stratigraphy of The
WCSB/TGI II FIELD TRIP SASKATCHEWAN/MANITOBA September 7-10th, 2004 MESOZOIC STRATIGRAPHY OF THE MANITOBA ESCARPMENT By J.D. Bamburak1 and J.E. Christopher2 1 Manitoba Geological Survey Manitoba Industry, Economic Development and Mines 360-1395 Ellice Avenue Winnipeg, MB., R3G 3P2 2 Saskatchewan Geological Survey Saskatchewan Industry and Resources 201 Dewdney Avenue Regina, SK., S4N 4G3 Figure 1: Manitoba Escarpment and upland components. Left – LANDSAT 7 mosaic. Bands 1, 2, and 3 (visible spectrum) were assigned to the colours blue, green, and red (respectively), resulting in a close to real colour image. Cultural elements (roads and township grid) and geographic elements (rivers) were added to each image. Right – Location map from McNeil and Caldwell (1981). PART I: STRATIGRAPHIC SETTING INTRODUCTION McNeil and Caldwell (1981) defined the Manitoba Escarpment (Fig. 1) as being composed mainly of Cretaceous rocks that form part of the eastern erosional edge of the Western Canada Sedimentary Basin- a composite feature which includes both the Elk Point Basin, centered in south-central Saskatchewan (which controlled Devonian deposition), and the Williston Basin, centered in northwestern North Dakota (which controlled the depositional patterns throughout the remainder of post-Cambrian time). The escarpment extends for 675 km from the Pasquia Hills in Saskatchewan, across southwestern Manitoba, to the Pembina Mountain area of North Dakota. The escarpment ranges in relief from a height from 442 m in the Pasquia Hills to 90 m to Pembina Mountain in North Dakota. The escarpment forms the irregular riser between the First Prairie Level on the Manitoba Lowlands and the second step, which forms Second Prairie Level to the west (Fig. -
Lower to Middle Paleozoic Stratigraphy of Southwestern Manitoba R
Electronic Capture, 2008 The PDF file from which this document was printed was generated by scanning an original copy of the publication. Because the capture method used was 'Searchable Image (Exact)', it was not possible to proofread the resulting file to remove errors resulting from the capture process. Users should therefore verify critical information in an original copy of the publication. © 1996: This book, or portions of it, may not be reproduced in any form without written permission ofthe Geological Association of Canada, Winnipeg Section. Additional copies can be purchased from the Geological Association of Canada, Winnipeg Section. Details are given on the back cover. TABLE OF CONTENTS INTRODUCTION TO THE PALEOZOIC STRATIGRAPHY OF SOUTHERN MANITOBA - PART I 1 ORDOVICIAN DEPOSITIONAL FRAMEWORK 6 Relationship of Outcrop Stops to Regional Depositional Framework 12 Ordovician Correlation and Nomenclature Problems 13 Possible Basement Control of Lower Paleozoic Tectonic Framework 14 SILURIAN DEPOSITIONAL FRAMEWORK 15 Silurian Correlation Problems 19 DEVONIAN DEPOSITIONAL FRAMEWORK 20 Elk Point Group 20 Lower Winnipegosis (Elm Point) Formation 27 Upper Winnipegosis Formation 28 Relationship of Outcrop Stops to the Regional Depositional Framework 31 Salt Collapse Structures 33 Winnipegosis Reef Morphology (Subsurface) Swan River Area 36 Effects of Reef Morphology on Outcrop Patterns 42 Detailed Reef Morphology, Outcrop Belt 43 Internal Structure of Reefs and Implications for Pattern of Reef Growth 44 Supplemental Notes Based on Recent Corehole Data 48 Steeprock Bridge Reef 48 Salt Point Reef Complex - Dawson Bay Area 48 Winnipegosis Area - Paradise Beach Reef Complex 50 The Narrows Area 52 Post-Reef Erosion, Sedimentation, and Diagenesis 53 Dawson Bay Formation 54 Souris River Formation 56 Point Wilkins Member 56 Sagemace Member 56 Possible Basement Control of Devonian Tectonic Framework 57 PALEOTECTONIC FRAMEWORK: A FOOTNOTE 58 GENERAL ROADLOG AND OUTCROP DESCRiPTIONS 59 PART II 59 DAY 1 59 ORDOVICIAN AND SILURIAI\! STRATIGRAPHY OF SOUTHERN MANITOBA. -
Brachiopoda)In Central and Western North America
Distribution of latest Givetian-Frasnian Atrypida (Brachiopoda)in central and western North America .TED DAY Day, J. 1998. Distribution of latest Givetian-Frasnian Atrypida (Brachiopoda) in central and western North America. -Acta Palaeontologica Polonica 43, 2,205-240. Diverse atrypid brachiopod faunas characterize very late Givetian-early Frasnian de- posits of Devonian Transgressive-Regressive (T-R) cycle IIb in North America which feature species of Desquamatia (Seratrypa), Desquamatia (Independatrypa), Pseudoat- rypa, Radiatrypa, Spinatrypina (S.), S. (Exatrypa), Spinatrypa (S.), Davidsonia, and possibly Iowatrypa Middle Frasnian faunas are not well documented in much of North America. Middle Frasnian deposits of T-R cycle IIc in the Great Basin, Iowa, and the southern Northwest Territories and Mackenzie shelf feature species of Neatrypa, Pseu- doatrypa, Radiatrypa, D. (Seratrypa), Spinatrypa, and possibly Costatrypa. Radiatrypa does not carry over into late Frasnian rocks of T-R cycle IId in North America. Genera common to late Frasnian deposits of T-R cycle IId-1 in central and western North America include widespread species of Pseudoatrypa, Spinatrypa, Costatrypa, Iowatrypa. D. (Seratrypa) and Neatrypa were restricted to the tropical platforms of western Canada at that time. Very late Frasnian brachiopod faunas of T-R cycle IId-2 yield species of Pseudoatrypa, Spinatrypa, Iowatrypa, and Pseudoatrypa? (southwest US only). Avail- able data on Late Frasnian brachiopod records in North American subtropical platforms (New Mexico and Iowa) indicate that two successive stepped late Frasnian extinction events affected those faunas, coinciding with the Lower Kellwasser Event and the Frasnian-Famennian (F-F) Event. Over half of the atrypid genera represented in late Frasnian North American faunas survived the first wave of extinctions (Lower Kell- wasser Event). -
Lower to Middle Paleozoic Stratigraphy of Southwestern Manitoba
WCSB/TGI II FIELD TRIP WINNIPEG, MANITOBA LOWER TO MIDDLE PALEOZOIC STRATIGRAPHY OF SOUTHWESTERN MANITOBA By R. K. Bezys and J. D. Bamburak Manitoba Geological Survey Industry, Trade and Mines 360-1395 Ellice Ave. Winnipeg, MB, R3G 3P2 ii LOWER TO MIDDLE PALEOZOIC STRATIGRAPHY OF SOUTHWESTERN MANITOBA PART I INTRODUCTION This field trip is designed to cover most of the accessible Ordovician, Silurian and Devonian outcrops in southwestern Manitoba. Ordovician and Silurian outcrops are examined on the first day; the more remote Devonian outcrops, of the Lake Winnipegosis - Lake Manitoba area, are examined on the second to fourth days. The stratigraphic nomenclature chart for southern Manitoba is shown in Figure 1. The Paleozoic outcrop belt of Manitoba occurs within the Manitoba Lowland or First Prairie Level (Figures 2 and 3). The Paleozoic succession dips gently to the southwest at approximately 2.8 m per km. South of the City of Winnipeg, within the Manitoba Lowland, a large area of Jurassic rocks occur as infill of a major pre-Mesozoic channel in the Paleozoic erosion surface. The Manitoba Lowland is bounded on the east by the Precambrian Shield, and on the west by the Manitoba Escarpment. The Escarpment forms the eastern edge of the Second Prairie Level, which is underlain by Cretaceous strata dipping gently to the southwest at 1.5 to 1.9 m per km. The actual Escarpment is composed of soft, easily eroded sands and shales in the lower part of the Cretaceous, underlying a resistant shale cap (Odanah Member of the Pierre Shale). The Manitoba outcrop belt is located on the northeastern edge of the Western Canada Sedimentary Basin - a composite feature which includes both the Elk Point Basin, centered in south-central Saskatchewan (which controlled Devonian deposition), and the Williston Basin, centered in northwestern North Dakota (which controlled the depositional patterns throughout the remainder of post-Cambrian time) (Fig. -
The Stratigraphy and Oil Activites of the Williston Basin in Southwestern
University of North Dakota UND Scholarly Commons Undergraduate Theses and Senior Projects Theses, Dissertations, and Senior Projects 1955 The trS atigraphy and Oil Activites of the Williston Basin in Southwestern Manitoba Wilfred M. DeYaegher Follow this and additional works at: https://commons.und.edu/senior-projects Recommended Citation DeYaegher, Wilfred M., "The trS atigraphy and Oil Activites of the Williston Basin in Southwestern Manitoba" (1955). Undergraduate Theses and Senior Projects. 1. https://commons.und.edu/senior-projects/1 This Thesis is brought to you for free and open access by the Theses, Dissertations, and Senior Projects at UND Scholarly Commons. It has been accepted for inclusion in Undergraduate Theses and Senior Projects by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. THE STRATIGRAPHY AND OIL ACTIVITIES OF THE WILLISTON BASTii lN SOUTHWESTERN MANITOBA A senior thesis submitted to the Staff of the Department of Geology University of North Dakota 1n partial fullf1llment of the requirements for the degree of e BACHELOR OF SCIENCE February 23,1955 by \-lilfred !~urice De Yaegher Grade REFERENCE DO NOT REMOVE fROM LJ BRARY Contents LJ.c:at~on and S1ze •••••••••..•...•• . .. 1 H.1story of 011 Act1v1tis: 1n The Williston Ba.sin. l Act1v1t1es 1h The United States ••.••••..••• ·••••••.•• • •••. 3 Canadian Activities •.•.••. 4 S.tr-a:tigraphy of Manitoba •• . .. .. .. 6 Oil Fields 1n Lani toba •••. .. .. .. .17 ., Conclusions ••••••••••.•••. ................................ .19 -1- The Stratigraphy and 011 Activities of the Williston Basin in Southwestern Manitoba The purpose of this paper is to give the general stratig raphic succession and oil activities within the Williston Basin in the United States and C,ui.ada. -
Potash Deposits in the Devonian Prairie Evaporite, Southwestern Manitoba Lo Eo Gic G a a L B S O U
Potash deposits in the Devonian Prairie Evaporite, southwestern Manitoba lo eo gic g a a l b s o u t r i v n e a MGS y m M.P.B. Nicolas 1928 Manitoba Geological Survey, Winnipeg, Manitoba, Canada Potash Geology 2. Regional and Local Geology 3. Esterhazy Member Potash Exploration In Manitoba, the Paleozoic-, Mesozoic- and Cenozoic-age strata form a basinward-thickening, southwesterly-sloping The Esterhazy Member is the most economic potash wedge, with the strata reaching a total thickness of 2.3 km in the extreme southestern corner of Manitoba (Figure 4). The beds. It consists of euhedral to subhedal halite crystals potash-bearing Devonian-age Prairie Evaporite was deposited within the Elk Point Basin (Figure 5). The Prairie Evaporite with large anhedral sylvite crystals and minor interstitial consists mainly of thick halite beds, with minor anhydrite and four localized potash beds. Within the basin, the formation carnolite and clays (Figure 7 and 8). 6. Potash Resource 1. Introduction can exceed 210 m in thickness, and lies at depths of 200 to 2,700 m below surface. 7. Exploration History The Esterhazy Member is intermittently present in a The Prairie Evaporite is a thick Denonian-aged evaporitic Legend R29W1 R28 R27 R26 R25 R24 R23 Formal mineral resource estimates have been prepared for the T30 The overlying Second Red Bed Member of the Dawson Bay Formation consists of grey, brown and red shales and narrow, elongate strip in southwestern Manitoba, from The discovery of potash in Manitoba was in an oil well drilled in sequence dominantly consisting of halite and anhydrite. -
GS2018-12: Lithostratigraphy of the Neepawa DDH No. 1 Prov. Core At
Lithostratigraphy of the Neepawa DDH No. 1 Prov. core at GS2018-12 15-29-14-14W1, southwestern Manitoba (part of NTS 62J3) by K. Lapenskie and M.P.B. Nicolas In Brief: Summary • Examination of nearly 500 m of Paleozoic strata from drill- Drillcore Neepawa DDH No. 1 Prov. 15-29-14-14W1, drilled in the vicinity of the town core Neepawa DDH allowed of Neepawa, provides a rare view of the entire lower Paleozoic section in the subsurface for positive correlations from the deep subsurface to of southwestern Manitoba. Terminating in Precambrian iron formation, this core consists outcrop belt, and indicates of 491.10 m of continuous core from the Ordovician Winnipeg Formation to the Devo- that additional studies may lead to the resolution of the nian Souris River Formation. Correlations of established outcrop-based lithostratigraphic stratigraphic framework of Manitoba units were extrapolated to the subsurface in Manitoba and, where established, mostly • Refining and resolving Paleo- Manitoba-derived lithostratigraphic units and nomenclature are used. Several correla- zoic stratigraphy of Manitoba has positive implications tion issues were resolved within this core and inconsistencies were identified, which indi- for petroleum and indus- cates that through additional study of drillcore and outcrop these issues may be resolved trial mineral industries, and carbonate-hosted lead-zinc Manitoba-wide. Refining the stratigraphic framework of the Williston Basin has positive mineralization exploration implications for the petroleum and industrial mineral industries and for Mississippi Val- ley–type deposit exploration. Citation: Lapenskie, K. and Nicolas, M.P.B. Introduction 2018: Lithostratigraphy of the In 1978, Neepawa Mines Ltd.