Helium in Southwestern Saskatchewan: Accumulation and Geological Setting
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PIPELINE FOODS, LLC, Et Al.,1 Debtors. Chapter 11 Case
Case 21-11002-KBO Doc 110 Filed 07/23/21 Page 1 of 54 IN THE UNITED STATES BANKRUPTCY COURT FOR THE DISTRICT OF DELAWARE In re: Chapter 11 PIPELINE FOODS, LLC, et al.,1 Case No. 21-11002 (KBO) Debtors. Jointly Administered AFFIDAVIT OF SERVICE I, Sabrina G. Tu, depose and say that I am employed by Stretto, the claims and noticing agent for the Debtors in the above-captioned cases. On July 21, 2021, at my direction and under my supervision, employees of Stretto caused the following documents to be served via overnight mail on the service list attached hereto as Exhibit A, and via electronic mail on the service list attached hereto as Exhibit B: • Notice of Telephonic Section 341 Meeting (Docket No. 73) • Application of the Debtors for Entry of an Order Pursuant to Bankruptcy Code Section 327(a), Bankruptcy Rules 2014(a) and 2016, and Local Rules 2014-1 and 2016- 2, Authorizing Appointment of Bankruptcy Management Solutions, Inc. d/b/a Stretto as Administrative Agent to the Debtors, Effective as of the Petition Date (Docket No. 85) • Motion of the Debtors for the Entry of an Order Authorizing (I) Retention and Employment of SierraConstellation Partners, LLC to Provide Interim Management Services, a Chief Restructuring Officer, and Additional Personnel, and (II) the Designation of Winston Mar as Chief Restructuring Officer, Effective as of the Petition Date (Docket No. 86) • Debtors’ Motion for Entry of Order Authorizing Debtors to Retain and Compensate Professionals Utilized in the Ordinary Course of Business, Effective as of the Petition Date (Docket No. -
Saskatchewan Intraprovincial Miles
GREYHOUND CANADA PASSENGER FARE TARIFF AND SALES MANUAL GREYHOUND CANADA TRANSPORTATION ULC. SASKATCHEWAN INTRA-PROVINCIAL MILES The miles shown in Section 9 are to be used in connection with the Mileage Fare Tables in Section 6 of this Manual. If through miles between origin and destination are not published, miles will be constructed via the route traveled, using miles in Section 9. Section 9 is divided into 8 sections as follows: Section 9 Inter-Provincial Mileage Section 9ab Alberta Intra-Provincial Mileage Section 9bc British Columbia Intra-Provincial Mileage Section 9mb Manitoba Intra-Provincial Mileage Section9on Ontario Intra-Provincial Mileage Section 9pq Quebec Intra-Provincial Mileage Section 9sk Saskatchewan Intra-Provincial Mileage Section 9yt Yukon Territory Intra-Provincial Mileage NOTE: Always quote and sell the lowest applicable fare to the passenger. Please check Section 7 - PROMOTIONAL FARES and Section 8 – CITY SPECIFIC REDUCED FARES first, for any promotional or reduced fares in effect that might result in a lower fare for the passenger. If there are none, then determine the miles and apply miles to the appropriate fare table. Tuesday, July 02, 2013 Page 9sk.1 of 29 GREYHOUND CANADA PASSENGER FARE TARIFF AND SALES MANUAL GREYHOUND CANADA TRANSPORTATION ULC. SASKATCHEWAN INTRA-PROVINCIAL MILES City Prv Miles City Prv Miles City Prv Miles BETWEEN ABBEY SK AND BETWEEN ALIDA SK AND BETWEEN ANEROID SK AND LANCER SK 8 STORTHOAKS SK 10 EASTEND SK 82 SHACKLETON SK 8 BETWEEN ALLAN SK AND HAZENMORE SK 8 SWIFT CURRENT SK 62 BETHUNE -
Saskatchewan Regional Newcomer Gateways
Saskatchewan Regional Newcomer Gateways Updated September 2011 Meadow Lake Big River Candle Lake St. Walburg Spiritwood Prince Nipawin Lloydminster wo Albert Carrot River Lashburn Shellbrook Birch Hills Maidstone L Melfort Hudson Bay Blaine Lake Kinistino Cut Knife North Duck ef Lake Wakaw Tisdale Unity Battleford Rosthern Cudworth Naicam Macklin Macklin Wilkie Humboldt Kelvington BiggarB Asquith Saskatoonn Watson Wadena N LuselandL Delisle Preeceville Allan Lanigan Foam Lake Dundurn Wynyard Canora Watrous Kindersley Rosetown Outlook Davidson Alsask Ituna Yorkton Legend Elrose Southey Cupar Regional FortAppelle Qu’Appelle Melville Newcomer Lumsden Esterhazy Indian Head Gateways Swift oo Herbert Caronport a Current Grenfell Communities Pense Regina Served Gull Lake Moose Moosomin Milestone Kipling (not all listed) Gravelbourg Jaw Maple Creek Wawota Routes Ponteix Weyburn Shaunavon Assiniboia Radwille Carlyle Oxbow Coronachc Regway Estevan Southeast Regional College 255 Spruce Drive Estevan Estevan SK S4A 2V6 Phone: (306) 637-4920 Southeast Newcomer Services Fax: (306) 634-8060 Email: [email protected] Website: www.southeastnewcomer.com Alameda Gainsborough Minton Alida Gladmar North Portal Antler Glen Ewen North Weyburn Arcola Goodwater Oungre Beaubier Griffin Oxbow Bellegarde Halbrite Radville Benson Hazelwood Redvers Bienfait Heward Roche Percee Cannington Lake Kennedy Storthoaks Carievale Kenosee Lake Stoughton Carlyle Kipling Torquay Carnduff Kisbey Tribune Coalfields Lake Alma Trossachs Creelman Lampman Walpole Estevan -
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 -
Sedimentology and Provenance of the Wood Mountain Formation and Derived Glacial and Glaciofluvial Sediments – Context for Kimberlite Indicator Mineral Anomalies
Preliminary Investigation: Sedimentology and Provenance of the Wood Mountain Formation and Derived Glacial and Glaciofluvial Sediments – Context for Kimberlite Indicator Mineral Anomalies Lynn Kelley and Gary Yeo Kelley, L. and Yeo, G. (2004): Preliminary investigation: Sedimentology and provenance of the Wood Mountain Formation and derived glacial and glaciofluvial sediments – context for kimberlite indicator mineral anomalies; in Summary of Investigations 2004, Volume 2, Saskatchewan Geological Survey, Sask. Industry Resources, Misc. Rep. 2004-4.2, CD-ROM, Paper A-12, 10p. Abstract Garnet, diopside, and chromite with chemistries inferred to indicate mantle affinity are geochemical pathfinders exploited in prospecting for diamond. In southern Saskatchewan, these minerals are found in high abundances in gravel, sand, and poorly-consolidated conglomerate of the Wood Mountain Formation, and overlying tills and glaciofluvial deposits. Several campaigns have been mounted to explore for a potential kimberlitic source for these pathfinder minerals, but no satisfactory explanation for their presence has been put forward. This project is intended to provide geological context for the occurrences of kimberlite indicator minerals found in the Wood Mountain area, by examining the transport history and provenance of the strata containing them. This note summarizes preliminary observations on sediment transport data and sediment provenance from seven locations. Grain size analysis, detailed provenance studies, and analysis for kimberlite indicator minerals and detrital gold are pending, and will be reported upon in a future communication. Keywords: Wood Mountain, kimberlite indicator, sediment provenance, paleocurrent. 1. Introduction a) Exploration History Southern Saskatchewan has been explored for diamond since at least 1963, when a De Beers affiliate discovered kimberlite indicator minerals in the Frenchman River Valley (Lehnert-Thiel et al., 1992). -
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. -
The Stonewall Formation Timothy O
The Stonewall Formation Timothy O. Nesheim Introduction Geology The Stonewall Formation is one of numerous sedimentary strata The Stonewall Formation consists of three carbonate-evaporitic that have commercially produced oil and gas from North Dakota’s cycles deposited during Late Ordovician through Early Silurian subsurface. The Stonewall Formation is also one of many time (fig. 2). The Stonewall Formation is conformably under- geological formations being overshadowed by the prolific Bakken- lain by the Stony Mountain Formation and overlain by the In- Three Forks play. Interestingly, the first successful production terlake Formation. Each Stonewall cycle consists of three gen- test that recovered hydrocarbons (oil and gas) from the eral lithofacies: 1) bioturbated to laminated carbonate mudstone Stonewall Formation took place in 1952, less than a year after the 2) thin greyish green dolomitic and/or shaley, silty to sandy discovery of oil in North Dakota. However, sustained commercial mudstone, and 3) nodular to laminated anhydrite that is some- production from the Stonewall Formation did not take place for times interlaminated to interbedded with dolomite (fig. 3). another 27 years until 1979. Since then, the Stonewall Formation Deposition is interpreted to have taken place within a shallow has produced approximately 10 million barrels of oil equivalent marine (carbonate facies) to hypersaline (anhydrite facies) set- (MBOE) from 65 vertical wells (fig. 1). ting. The shaly sandy mudstone intervals have previously been Figure 1. Map depicting the extent of the Stonewall Formation and Stonewall productive wells in North Dakota (Carlson and Eastwood, 1962). For regulatory reasons the Stonewall Formation has been pooled together with the lower Interlake Formation. -
Perspectives of Saskatchewan Dakota/Lakota Elders on the Treaty Process Within Canada.” Please Read This Form Carefully, and Feel Free to Ask Questions You Might Have
Perspectives of Saskatchewan Dakota/Lakota Elders on the Treaty Process within Canada A Dissertation Submitted to the College of Graduate Studies and Research In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy In Interdisciplinary Studies University of Saskatchewan Saskatoon By Leo J. Omani © Leo J. Omani, copyright March, 2010. All rights reserved. PERMISSION TO USE In presenting this thesis 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 the thesis in any manner, in whole or in part, for scholarly purposes may be granted by the professor or professors who supervised my thesis work or, in their absence, by the Head of the Department or the Dean of the College in which my thesis was completed. It is understood that any copying or publication or use of this thesis or parts thereof for financial gain is not to 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. Request for permission to copy or to make other use of material in this thesis, in whole or part should be addressed to: Graduate Chair, Interdisciplinary Committee Interdisciplinary Studies Program College of Graduate Studies and Research University of Saskatchewan Room C180 Administration Building 105 Administration Place Saskatoon, Saskatchewan Canada S7N 5A2 i ABSTRACT This ethnographic dissertation study contains a total of six chapters. -
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 -
Silurian System in Eastern Montana
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1966 Silurian system in eastern Montana Frank Kendall Gibbs The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Gibbs, Frank Kendall, "Silurian system in eastern Montana" (1966). Graduate Student Theses, Dissertations, & Professional Papers. 9265. https://scholarworks.umt.edu/etd/9265 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. THE SILURIAN SYSTEM IN EASTERN MONTANA by Frank Kendall Gibbs Geological Bhgineer Colorado School Of Mines, 1955 Presented in partial fulfillment of the requirements for the degree of Master of Science U niversity of Montana 1966 Approved by: 1 Chairman, Board of Examiners Deary" Graduate School J A r r c '^’^ -7_____________ Date ( i ) UMI Number: EP40067 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMT Dissertation PuWisNng UMI EP40067 Published by ProOuest LLC (2013). Copyright in the Dissertation held by the Author. Microform Edition © ProOuest LLC.