MIE HOLDINGS CORPORATION MI能源控股有限公司 (Incorporated in the Cayman Islands with Limited Liability) (Stock Code: 1555)

Total Page:16

File Type:pdf, Size:1020Kb

MIE HOLDINGS CORPORATION MI能源控股有限公司 (Incorporated in the Cayman Islands with Limited Liability) (Stock Code: 1555) THIS CIRCULAR IS IMPORTANT AND REQUIRES YOUR IMMEDIATE ATTENTION If you are in any doubt as to any aspect of this circular or as to the action to be taken, you should consult your licensed securities dealer, bank manager, solicitor, professional accountant or other professional adviser. If you have sold or transferred all your shares in MIE Holdings Corporation, you should at once hand this circular to the purchaser or transferee or to the bank, licensed securities dealer or other agent through whom the sale or transfer was effected for transmission to the purchaser or transferee. Hong Kong Exchanges and Clearing Limited and The Stock Exchange of Hong Kong Limited take no responsibility for the contents of this circular, make no representation as to its accuracy or completeness and expressly disclaim any liability whatsoever for any loss howsoever arising from or in reliance upon the whole or any part of the contents of this circular. MIE HOLDINGS CORPORATION MI能源控股有限公司 (Incorporated in the Cayman Islands with limited liability) (Stock Code: 1555) VERY SUBSTANTIAL DISPOSAL AND CONNECTED TRANSACTION IN RELATION TO THE PROPOSED DISPOSAL OF ENTIRE EQUITY INTEREST IN MAPLE MARATHON AND NOTICE OF EXTRAORDINARY GENERAL MEETING Independent Financial Adviser to the Independent Board Committee and the Independent Shareholders A letter from the Board is set out on pages 6 to 19 of this circular and a letter from the Independent Board Committee containing its recommendation to the Independent Shareholders is set out on pages 20 to 21 of this circular. A letter from the Independent Financial Adviser containing its recommendation to the Independent Board Committee and the Independent Shareholders is set out on pages 22 to 57 of this circular. A notice convening the EGM of MIE Holdings Corporation to be held at Room 13, 7/F, Nexxus Building, 77 Des Voeux Road Central, Hong Kong on Tuesday, November 20, 2018 at 10:00 a.m. or any adjournment thereof is set out on pages EGM-1 to EGM-2 of this circular. A form of proxy for use at the EGM is also enclosed. Such form of proxy is also published on the websites of Hong Kong Exchanges and Clearing Limited (http://www.hkexnews.hk) and the Company (http://www.mienergy.com.cn). Whether or not you are able to attend and vote at the EGM, please complete and sign the enclosed form of proxy in accordance with the instructions printed thereon and return it to the Company’s branch share registrar in Hong Kong, Tricor Investor Services Limited, at Level 22, Hopewell Centre, 183 Queen’s Road East, Hong Kong as soon as possible but in any event not less than 48 hours before the time appointed for the holding of the EGM or any adjournment thereof. Completion and return of the form of proxy as instructed will not preclude you from attending andvotinginpersonattheEGMifyousowish. November 5, 2018 CONTENTS Page DEFINITIONS ................................................................. 1 LETTER FROM THE BOARD ................................................. 6 LETTER FROM THE INDEPENDENT BOARD COMMITTEE ................ 20 LETTER FROM THE INDEPENDENT FINANCIAL ADVISER ............... 22 APPENDIX I — FINANCIAL INFORMATION OF THE GROUP ............ I-1 APPENDIX II — FINANCIAL INFORMATION OF THEDISPOSALGROUP ................................. II-1 APPENDIX III — UNAUDITED PRO FORMA FINANCIAL INFORMATION OF THE REMAINING GROUP .......................... III-1 APPENDIX IV — COMPETENT PERSON’SREPORT ........................ IV-1 APPENDIX V — GENERAL INFORMATION ................................ V-1 NOTICE OF EGM ............................................................. EGM-1 – i – DEFINITIONS In this circular, the following expressions have the following meanings unless the context otherwise requires: ‘‘Acquisition’’ the very substantial acquisition of CQ Energy Canada Partnership by Canlin which was completed on September 29, 2017 as announced by the Company on June 9, 2017 and October 3, 2017 ‘‘Announcement the announcement dated September 24, 2018 made by the Company in relation to the Disposal ‘‘associate(s)’’ has the meaning ascribed to it under the Listing Rules ‘‘Board’’ the board of Directors of the Company ‘‘C$’’ Canadian Dollars, the lawful currency of Canada ‘‘Canlin’’ Canlin Energy Corporation, a corporation incorporated in British Columbia, Canada whose entire share capital of common shares are held by Maple Marathon as at the date of this circular ‘‘Company’’ MIE Holdings Corporation (stock code: 1555), a company incorporated in the Cayman Islands with limited liability on March 20, 2008, the ordinary shares of which are listed on the Main Board of the Stock Exchange ‘‘Competent Person’’ Sproule Associates Limited ‘‘Competent Person’s Report’’ the competent person’s report, which is set out in ‘‘Appendix IV — Competent Person’s Report’’ of this circular, prepared by the Competent Person in accordance with the Listing Rules ‘‘Competition Act’’ the Competition Act (Canada), R.S.C. 1985, c. C-34, as amended ‘‘connected person(s)’’ has the meaning ascribed to it under the Listing Rules ‘‘Consideration’’ the consideration of US$250,000,000 (equivalent to approximately HK$1,961,950,000) payable by Far East Energy to the Company in accordance with the Share Purchase Agreement ‘‘controlling shareholder’’ has the meaning ascribed to it under the Listing Rules ‘‘Director(s)’’ director(s) of the Company – 1 – DEFINITIONS ‘‘Disposal’’ the proposed disposal of 100 issued shares of Maple Marathon, representing its entire issued share capital, by MIEJ to Far East Energy pursuant to the Share Purchase Agreement ‘‘Disposal Group’’ Maple Marathon and its subsidiaries collectively ‘‘EGM’’ the extraordinary general meeting of the Company to be convened on November 20, 2018 to consider and, if thought fit, approve, among others, the Share Purchase Agreement and the transaction contemplated thereunder ‘‘Far East Energy’’ Far East Energy International Limited, a limited company incorporated in the British Virgin Islands indirectly wholly owned by Mr. Zhang as at the date of this circular ‘‘FEEL’’ Far East Energy Limited, a limited company incorporated in Hong Kong and a substantial shareholder of the Company, held by Mrs. Zhang, Mr. Zhang and Mr. Zhao Jiangwei as to 80%, 9.99% and 10%, respectively, where Mrs. Zhang, Mr. Zhang and Mr. Zhao Jiangwei have entered into an acting-in-concert agreement under which Mr. Zhang is allowed to vote on his, Mrs. Zhang’s and Mr. Zhao’sshares if a unanimous opinion in relation to the matters that requires action in concert is unable to be reached ‘‘FY2014’’ the financial year of the Company ended December 31, 2014 ‘‘FY2015’’ the financial year of the Company ended December 31, 2015 ‘‘FY2016’’ the financial year of the Company ended December 31, 2016 ‘‘FY2017’’ the financial year of the Company ended December 31, 2017 ‘‘1H2018’’ the six months of the Company ending June 30, 2018 ‘‘Group’’ the Company and its subsidiaries ‘‘HK$’’ Hong Kong dollars, the lawful currency of Hong Kong ‘‘Hong Kong’’ the Hong Kong Special Administrative Region of the PRC ‘‘IFRS’’ International Financial Reporting Standards issued by the International Accounting Standards Board which is in effect – 2 – DEFINITIONS ‘‘Independent Board an independent committee of the Board formed to advise Committee’’ the Independent Shareholders in respect of the Disposal, comprising all independent non-executive Directors, namely, Mr. Mei Jianping, Mr. Jeffrey Willard Miller and Mr. Guo Yanjun ‘‘Independent Financial Platinum Securities Company Limited, a corporation Adviser’’ licensed to carry out type 1 (dealing in securities) and type 6 (advising on corporate finance) regulated activities under the SFO, being the independent financial adviser appointed to advise the Independent Board Committee and the Independent Shareholders in respect of the Share Purchase Agreement and the transactions contemplated thereunder ‘‘Independent Shareholders’’ the Shareholders other than FEEL and its associates ‘‘Latest Practicable Date’’ November 1, 2018, being the latest practicable date prior to the publication of this circular for ascertaining certain information contained herein ‘‘Listing Rules’’ the Rules Governing the Listing of Securities on the Stock Exchange, as amended, supplemented or otherwise modified from time to time ‘‘Maple Marathon’’ Maple Marathon Investments Limited, a limited company incorporated in Hong Kong and a wholly owned subsidiary of the Company as at the date of this circular ‘‘mcf’’ one thousand cubic feet ‘‘MIEJ’’ MIE Jurassic Energy Corporation, a company incorporated under the laws of Cayman Islands, wholly owned by the Company as at the date of this circular ‘‘MMBOE’’ million barrels of oil equivalent ‘‘Mr. Zhang’’ Mr. Zhang Ruilin, the Chairman, an executive Director and a substantial shareholder of the Company ‘‘Mrs. Zhang’’ Ms. Zhao Jiangbo, the spouse of Mr. Zhang Ruilin and a substantial shareholder of the Company ‘‘No Action Letter’’ a communication in writing from the Commissioner of Competition advising that he or she does not, at the present time, intend to make an application to the Competition Tribunal under Section 92 of the Competition Act in respect of the transactions contemplated hereunder – 3 – DEFINITIONS ‘‘Outstanding Debts’’ the outstanding debts of the Company due in the 12 months from the Latest Practicable Date at the total amount of US$470,000,000 (equivalent to approximately HK$3,688,466,000) ‘‘Outstanding Intra-Group means all intra-group debts owed by the Maple Marathon to Debts’’
Recommended publications
  • L'.3350 Deposmon and DISSOLUTION of the MIDDLE DEVONIAN PRAIRIE FORMATION, Williston BASIN, NORTH DAKOTA and MONTANA By
    l'.3350 DEPOsmON AND DISSOLUTION OF THE MIDDLE DEVONIAN PRAIRIE FORMATION, WilLISTON BASIN, NORTH DAKOTA AND MONTANA by: Chris A. Oglesby T-3350 A thesis submined to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Master of Science (Geology). Golden, Colorado Date f:" /2 7 /C''i::-- i ; Signed: Approved: Lee C. Gerhard Thesis Advisor Golden, Colorado - 7 Date' .' Samuel S. Adams, Head Department of Geology and Geological Engineering II T-3350 ABSTRACf Within the Williston basin, thickness variations of the Prairie Formation are common and are interpreted to originate by two processes, differential accumulation of salt during deposition, and differential removal of salt by dissolution. Unambiguous evidence for each process is rare because the Prairie/Winnipegosis interval is seldom cored within the U.S. portion of the basin. Therefore indirect methods, utilizing well logs, provide the principal method for identifying characteristics of the two processes. The results of this study indicate that the two processes can be distinguished using correlations within the Prairie Formation. Several regionally correlative upward-brining, and probably shoaling-upward sequences occur within the Prairie Formation .. Near the basin center, the lowermost sequence is transitional with the underlying Winnipegosis Formation. This transition is characterized by thinly laminated carbonates that become increasingly interbedded with anhydrites of the basin-centered Ratner Member, the remainder of the sequence progresses up through halite and culminates in the halite-dominated Esterhazy potash beds. Two overlying sequences also brine upwards, however, these sequences lack the basal anhydrite and instead begin with halite and culminate in the Belle Plaine and Mountrail potash Members, respectively.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • National Advisory Committee on Research in the Geological Sciences
    6 -01 NATIONAL ADVISORY COMMITTEE ON RESEARCH IN THE GEOLOGICAL SCIENCES SIXTEENTH ANNUAL REPORT 1965-66 ANNUAL REVIEW AND REPORTS OF SUBCOMMITTEES Published by the Geological Survey of Canada as GSC Paper 66 -61 MANUSCRIPT AI'1D National Advisory Cf\ DT()':~AO~JY - APR 3 1967 HR · 1967 Price, 5 D ce nts 1967 SECTION Comn-.:!:~ee SIXTEENTH ANNUAL REPORT 1965-66 ANNUAL REVIEW AND REPORTS OF SUBCOMMITTEES @ Crown C opyrights reserved Availa b le by mail from the Queen' s Printer, Otta wa from the Geologi cal Survey of Canada, 601 B ooth St. , Ottawa and a t th e fo llowing Can a dian Governm ent book s h op s: OTTAWA Daly Building, Corner Mackenzie and Rideau TORONTO 221 Yonge Street MONTREAL /Eterna-Vie Building, 1182 St. Catherine St. West WINNIPEG Mall Center Building, 499 Portage Avenue VANCOUVER 657 Granville Avenue HALIFAX 1737 Barrington Street or through your bookseller A deposit copy of this publication is also available for reference in public libraries across Canada Price, 50 cents Cat. No. M44-66-61 Price subject to change without notice ROGER D UHAMEL, F.R.S.C. Queen's Printer and Controller of Stationery Ottawa, Canada 1967 CONTENTS Page MEMBERS OF COMMITTEE . • . • . • • . • . • . • . • • . vii Executive Committee . • . • . • . • • . • • • • . • . viii Projects Subcommittee . • . • . • . • . • • . • • • • • • • • . • . • • • • ix THE YEAR IN REVIEW •.....•.•••••...••••......•..•..•..•..•.• Research grants to universities .•.•••...••.........•....••• Comprehensive studies of Canadian sulphide • • . • . • • . • . • . • . • Z Storage and retrieval of geological data . • . • . • • • . • 3 Geochemical prospecting symposium........................ 6 International Union of Geological Sciences . • . • . • • . • • . • . • . 6 Summary statements and discussion of subcommittee reports.. 7 Changes in personnel of committee ....................... 13 SUBCOMMITTEE REPORTS..................................... 14 Geophysical methods applied to geological problems .
    [Show full text]
  • 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 3. Esterhazy Member The Esterhazy Member is the most economic Potash Exploration potash beds. It consists of euhedral to subhedal halite 2. Regional and Local Geology crystals with large anhedral sylvite crystals and minor 1. Introduction interstitial carnolite and clays (Figure 7 and 8). In Manitoba, the Paleozoic-, Mesozoic- and Cenozoic-age strata form a basinward-thickening, southwesterly- 6. Potash Resource 7. Exploration History The Prairie Evaporite is a thick Denonian-aged evaporitic sloping wedge, with the strata reaching a total thickness of 2.3 km in the extreme southestern corner of Manitoba The Esterhazy Member is intermittently present in R29W1 R28 R27 R26 R25 R24 R23 sequence dominantly consisting of halite and anhydrite. It Legend (Figure 4). The potash-bearing Devonian-age Prairie Evaporite was deposited within the Elk Point Basin (Figure Formal mineral resource estimates have been prepared for The discovery of potash in Manitoba was in an oil well T30 a narrow, elongate strip in southwestern Manitoba, includes four potash-bearing members, from oldest to youngest N 5). The Prairie Evaporite consists mainly of thick halite beds, with minor anhydrite and four localized potash beds. the Russell deposit, most recently in 2009. A historical resource drilled in 1951 at 15-18-10-27W1. This discovery led to salt distribution WA T29 from Township 5 to 21, Ranges 27 to 29 W1 (Figure E A H B C Within the basin, the formation can exceed 210 m in thickness, and lies at depths of 200 to 2,700 m below surface.
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • Occurrences of CO2 Within Southwest Saskatchewan: Natural Analogues
    Occurrences of CO2 within Southwest Saskatchewan: Natural 1 Analogues to the Weyburn CO2 Injection Site John Lake 2 and Steve Whittaker Lake, J. and Whittaker, S. (2006): Occurrences of CO2 within southwest Saskatchewan: Natural analogues to the Weyburn CO2 injection site; in Summary of Investigations 2006, Volume 1, Saskatchewan Geological Survey, Misc. Rep. 2006-4.1, CD-ROM, Paper A-5, 14p. Abstract On the western flank of the Williston Basin in southwestern Saskatchewan, CO2 occurs in natural accumulations within Devonian carbonates and Cambrian siliciclastics. Inert gases from some carbonate reservoirs contain 3 greater than 80% CO2 and have sustained flow rates up to 425 000 m /day. Early estimates of this resource suggested nearly two million tonnes of CO2 or about one billion cubic metres of recoverable gas are present in these rocks. These natural CO2 occurrences are found about 400 km west of the site of the IEA Weyburn CO2 Storage and Monitoring Project, which is directed toward assessing the potential for safe geological storage of anthropogenic CO2 in Mississippian carbonates. This study is focused on the Devonian natural CO2 accumulations because of geological similarity to the Weyburn injection site and because they contain the greatest amount of CO2. Inert gases in southwestern Saskatchewan, including variable amounts of N2, He, and CO2, are generally trapped in Devonian strata of the Duperow Formation within a succession of thin cycles of carbonates capped by evaporite units. The cycles resulted from deposition within shallow, periodically restricted waters along a carbonate platform. The strata vary from dolomitized limestones to limestones. Within reservoir intervals, porosities are generally around 6 to 8%, but may be as high as 18%.
    [Show full text]
  • 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.
    [Show full text]
  • The Duperow Formation, Williston Basin, North Dakota Zachary P
    University of North Dakota UND Scholarly Commons Theses and Dissertations Theses, Dissertations, and Senior Projects 2014 Lithostratigraphic investigation of a Late Devonian carbonate-evaporite sequence; the Duperow Formation, Williston Basin, North Dakota Zachary P. Alcorn University of North Dakota Follow this and additional works at: https://commons.und.edu/theses Part of the Geology Commons Recommended Citation Alcorn, Zachary P., "Lithostratigraphic investigation of a Late Devonian carbonate-evaporite sequence; the Duperow Formation, Williston Basin, North Dakota" (2014). Theses and Dissertations. 1. https://commons.und.edu/theses/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 Theses and Dissertations by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. LITHOSTRATIGRAPHIC INVESTIGATION OF A LATE DEVONIAN CARBONATE-EVAPORITE SEQUENCE; THE DUPEROW FORMATION, WILLISTON BASIN, NORTH DAKOTA by Zachary P. Alcorn Bachelor of Science in Geology, Marietta College, 2012 A Thesis Submitted to the Graduate Faculty of the University of North Dakota in partial fulfillment of the requirements for the degree of Master of Science Grand Forks, North Dakota August 2014 This thesis, submitted by Zachary P. Alcorn in partial fulfillment of the requirements for the Degree of Master of Science from the University of North Dakota, has been read by the Faculty Advisory Committee under whom the work has been done and is hereby approved. ________________________________________ Richard D. LeFever, Ph.D.,-Chairperson ________________________________________ Joseph Hartman, Ph.D.,-Committee Member ________________________________________ Nels Forsman, Ph.D.,-Committee Member This thesis is being submitted by the appointed advisory committee as having met all of the requirements of the School of Graduate Studies at the University of North Dakota and is hereby approved.
    [Show full text]
  • 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.
    [Show full text]