DOCSLIB.ORG

Red River Carbonates (Saskatchewan): Major Facies, Lithological, and Spatial Controls on Rock Magnetism – Preliminary Observations

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Red River Carbonates (Saskatchewan): Major Facies, Lithological, and Spatial Controls on Rock Magnetism – Preliminary Observations Red River Carbonates (Saskatchewan): Major Facies, Lithological, and Spatial Controls on Rock Magnetism – Preliminary Observations Erika Szabo 1 and Maria T. Cioppa 2 Szabo, E. and Cioppa, M.T. (2003): Red River carbonates (Saskatchewan): Major facies, lithological, and spatial controls on rock magnetism – preliminary observations; in Summary of Investigations 2003, Volume 1, Saskatchewan Geological Survey, Sask. Industry Resources, Misc. Rep. 2003-4.1, CD-ROM, Paper A-2, 9p. Abstract Preliminary results from ten wells in the Saskatchewan portion of the Williston Basin reveal significant lithological, facies, and spatial controls on the natural remanent magnetization (NRM) intensity in Red River carbonates. High NRM intensity values are recorded within the limestone sequences, intermediate values are seen in burrowed/fossiliferous dolostone, and the lowest values of NRM intensity are measured in laminated/bedded dolostones associated with anhydrite. The NRM intensity tends to increase towards the centre of the Williston Basin suggesting that the most probable variables affecting NRM intensities are: 1) depth of sampling and 2) proximity to the North American Central Plains Conductivity Anomaly. With a few exceptions, the magnetite grain-size distribution determined from partial anhysteretic remanent magnetization (pARM) spectra seems to be unaffected by facies and other lithological variations, or by spatial position. Well 0210, in the northwestern part of the Williston Basin, however, has magnetite grain-size values that are predominantly in the pseudosingle domain range whereas samples from the other wells display a mixed pseudosingle and single domain grain-size distribution. These findings suggest that fluid flow from the Alberta Basin may have influenced this portion of the Williston Basin. Keywords: Upper Ordovician, Williston Basin, Red River, Yeoman Formation, Herald Formation, Saskatchewan, rock magnetism, carbonates, facies control, lithological control, spatial control. 1. Introduction Paleomagnetic studies of several Paleozoic formations in the Alberta Basin indicate that paleomagnetic components of different ages can be correlated with lithological facies, and that detailed paleomagnetic and rock magnetic analyses can determine the order and timing of diagenetic events (Cioppa et al., 2001). Information on paleomagnetism in the Williston Basin is limited (e.g. Enkin et al., 2001; Cioppa, 2003); however, reliable paleomagnetic data obtained from preliminary studies in the basin (Cioppa, 2002, unpubl. data) suggest that further research is warranted. This paper presents preliminary results from a detailed paleomagnetic and rock magnetic investigation of Red River carbonates in Saskatchewan. We examine the potential for facies or spatial controls of paleomagnetic patterns in these rocks which are characterized by several different lithological facies and dolomitization events. 2. Geology The Williston Basin is ~800 km in diameter. It covers much of southern Saskatchewan and Manitoba in Canada and extends southward through Montana, North Dakota, and South Dakota in the United States (Figure 1). The Precambrian basement, which is reached at a maximum depth of ~5 km in North Dakota, features several structures that influence the generation and migration of hydrocarbons in the Williston Basin (Osadetz et al., 1992). The North American Central Plains Conductivity Anomaly (NACPCA, Figure 1), a 2000 km long and 80 km wide structure at a depth of 10 to 20 km, is characterized by basal heat flow that is ~20% higher than elsewhere in the basin (Jones and Craven, 1990; Jones and Savage, 1986). 1 Earth Sciences, University of Western Ontario, London, ON N6A 5B7; E-mail: [email protected]. 2 Department of Earth Sciences, University of Windsor, Windsor, ON N9B 3P4. Saskatchewan Geological Survey 1 Summary of Investigations 2003, Volume 1 Figure 1 - Distribution of Ordovician and Silurian strata within the Williston Basin with locations of sampled wells (NACPCA- North American Central Plains Conductivity Anomaly) (after Norford et al., 1994 and Morel-a-l’Huissier et al., 1990). Upper Ordovician Red River carbonates comprise the Yeoman and Herald formations (Norford et al., 1994). Within conformable limits, these formations are underlain by clastics of the Winnipeg Formation and overlain by carbonates of the Stony Mountain Formation. The Yeoman Formation is the thickest formation of the Red River carbonates. Various fossils and traces of different burrows are found in the Yeoman. The larger burrows are Thalassinoides-like structures that are thought to have been re-burrowed, as indicated by the smaller included burrows (i.e. Planolites, Chondrites) (Kendall 1976, 1977; Haidl et al., 1997; Canter, 1998; Pak et al., 2001). Several types of dolomitization are present in the Yeoman Formation. The burrows are commonly dolomitized, and may be associated with either a limestone or dolostone matrix. Also, minor saddle dolomite cement has been precipitated in vugs, fractures, and geopetal structures (Carroll, 1979; Qing et al., 2001). The Herald Formation is divided into the Lake Alma and Coronach members, and the overlying Redvers unit (Kendall, 1976). Laminated to bedded dolostones and calcareous dolostones, sometimes interbedded with burrowed or fossiliferous dolostones, lie beneath nodular, bedded, and laminated anhydrite with anhydritic dolostone Saskatchewan Geological Survey 2 Summary of Investigations 2003, Volume 1 interbeds in the Lake Alma Member (Nowlan and Haidl, 2001). From bottom to top, the Coronach Member is composed of argillaceous dolostones, fossiliferous and burrowed limestones and dolostones, laminated dolostones that are locally limestones, and an upper anhydrite (Kendall, 1976; Nowlan and Haidl, 2001). The base of the Redvers unit is argillaceous dolostone, which is overlain by an upper laminated dolostone or limestone (Nowlan and Haidl, 2001). In the Lake Alma Member of the Herald Formation, dolomitization is recognized in the form of non- porous cryptocrystalline and porous crystalline dolostone (Qing et al., 2001). 3. Methodology Systematic sampling, utilizing the paleomagnetic sampling procedure described by Lewchuk et al. (1998) and Cioppa et al. (2000), was carried out on core from ten wells in southern Saskatchewan (Table 1). Nine wells are located along two cross-section lines: one east-west (A-A’) and the second (B-B’) north-south (Figure 1). The tenth well (0210) was sampled in the west-central part of the province, removed from the other sampling locations (Figure 1). Detailed macroscopic lithological observations were made of each core. A total of 152 plugs, each 2.5 cm in diameter, were drilled from the well cores. From the core plugs, 434 specimens were cut. As the first phase of this project, we measured the natural remanent magnetization (NRM) of all specimens using a vertical- configuration 2G cryogenic magnetometer with a lower sensitivity limit of ~2x10-6 A/m. Thirty pilot specimens (2 to 4 specimens per well) were subjected to alternating field (AF) demagnetization before any rock magnetic experiments were performed. Results of these measurements will be presented in the near future. We also measured stepwise partial anhysteretic remanent magnetization (pARM) on the pilot samples by treating the specimens in steps of 10 mT up to 100 mT using the procedure introduced by Everitt (1961) and a Sapphire Instruments SI-4 Alternating Field (AF) demagnetizer. The AF and pARM demagnetization procedures differ in that the pARM procedure has a small biased direct circuit (DC) field applied over a section of the AF demagnetizing field (i.e. DC between 10 and 20 mT over AF demagnetization from 100 mT). The procedure is performed because coercivity is a function of grain size and by doing a step sequence of DC biases (0 to 10 mT, 10 to 20 mT, ... , 90 to 100 mT) an estimate is obtained of the relative amounts of magnetic grain sizes. The percentage of the different ranges of magnetic grain sizes is approximated by the measured pARM values and their corresponding grain size ranges as defined by Jackson et al. (1988). Thus, the magnetization intensity values for the untreated specimens are considered to represent the amount of multidomain (MD) size grains, the sum of pARM values obtained over the intervals 0 to 10 mT to 30 to 40 mT represent the amount of pseudosingle domain (PSD) particles, and the sum of the pARM values for the remaining intervals (40 to 50 mT to 90 to 100 mT) represent the amount of single domain (SD) magnetic particles. All experiments were done in a magnetically shielded room in the Paleomagnetics Laboratory at the University of Windsor (Canada). 4. Results and Preliminary Observations a) Natural Remanent Magnetization (NRM) The NRM intensities vary from well to well across the study area and also within individual wells with values ranging from 10-6 A/m to 10-2 A/m. NRM intensities of specimens cut from the outside of most plugs were systematically higher than those cut from the interior of the plug (e.g. for ~12% of the plugs, the outside specimens exceeded twice the NRM values from specimens from the middle of the plug). It is considered that the outer surface of a core, which would have been in direct contact with the core barrel, is much more likely to acquire a drilling- induced viscous magnetization than the interior of the core. Therefore, the analysis of the NRM intensity distribution was carried out only on specimens cut from the middle of the core plugs. Table 1 - List of sampled cores. Well Well Name Location Logged Interval (m) Formation Sampled 0201 Pan American White Bear Cres. 5-15-10-2W2 2148.1 to 2482.6 Herald and Yeoman 0202 Ceepee Annette 10-25-36-5W2 3083.0 to 3103.0 and Yeoman 3154.0 to 3164.0 0203 Esso Bromhead 6-28-3-12W2 2875.6 to 2893.6 Yeoman 0204 PCP Scurry et al Lake Alma 5-29-01-17W2 3071.0 to 3089.5 Herald and Yeoman 0205 Trilink Hazelwood 4-14-11-5W2 2225.0 to 2243.0 Yeoman 0206 Mark Saskoil Minton 1-10-3-21W2 2856.0 to 2874.0 Yeoman 0207 T.W. Wapella Cr. 12-34-14-1W2 1677.5 to 1692.8 Herald and Yeoman 0208 Imp.
Load more

Recommended publications
  • AND GEOLOGY of the SURROUNDING AREA I
    . " ... , - .: ~... GP3/10 ~ " . :6',;, J .~~- -i-~ .. '~ MANITOBA MINES BRANCH DEPARTMENT OF MfNES AND NATURAL RESOURCES LAKE ST. MARTIN CRYPTO~EXPLOSION CRATER .. AND GEOLOGY OF THE SURROUNDING AREA i . , - by H. R. McCabe and B. B. Bannatyne Geological Paper 3/70 Winnipeg 1970 Electronic Capture, 2011 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. (i) GP3/10 MANITOBA M]NES BRANCH DEPARTMENT OF MINES AND NATURAL RESOURCES LAKE ST. MARTIN CRYPTO·EXPLOSION CRATER AND GEOLOGY OF THE SURROUNDING AREA by H. R. McCabe and B. B. Bannatync • Geological Paper 3/70 Winnipeg 1970 (ii) TABLE OF CONTENTS Page Introduction' r Previous work I .. Present work 2 Purpose 4 Acknowledgcmcnts 4 Part A - Regional geology and structural setting 4 Post-Silurian paleogeography 10 Post-crater structure 11 Uthology 11 Precambrian rocks 12 Winnipeg Fomlation 13 Red River Fomlation 14 Stony Mountain Formation 15 Gunn Member 15 Gunton Member 16 Stoncwall Formation 16 Interlake Group 16 Summary 17 Part B - Lake St. Martin crypto-explosion crater 33 St. Martin series 33 Shock metamorphism 33 Quartz 33 Feldspar 35 Biotite 35 Amphibole 36 Pseudotachylyte 36 Altered gneiss 37 Carbonate breccias 41 Polymict breccias 43 Aphanitic igneous rocks - trachyandcsitc 47 Post·crater Red Beds and Evaporites (Amaranth Formation?) 50 Red Bed Member 50 Evaporite Member 52 Age of Red Bed·Evaporite sequence 53 Selected References 67 .
    [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]
  • Oil and Gas Potential of the Red River Formation, Southwestern North Dakota Timothy O
    Oil and Gas Potential of the Red River Formation, Southwestern North Dakota Timothy O. Nesheim Introduction North Dakota has experienced commercial oil and gas production third highest for the state, a bronze medal so to speak, and is from 19 different geologic formations over the past 65 years. only eclipsed by the “gold” medal Bakken-Three Forks Formations Most of these productive formations have experienced spotlight (>1.2 billion barrels of oil) and the “silver” medal Madison Group attention from the oil and gas industry at one time or another, (Mission Canyon & Charles Formations, ~1 billion barrels of oil). and, whether for a few months or years, were considered a “hot Red River production is also regionally extensive and stretches play” to explore and develop. The unconventional Bakken-Three into northwestern South Dakota, eastern Montana, and southern Forks development is a current example of a play that brought Saskatchewan (fig. 1). oil and gas activity in the state to record levels and has sustained drilling activity even in a depressed oil and gas market. As the Summary of Red River Oil and Gas Production oil and gas industry transitions beyond the Bakken over time and The upper Red River consists of four, vertically stacked, oil- begins to spend more time evaluating the other 17 productive productive sedimentary rock layers referred to informally as the non-Bakken/Three Forks Formations, additional oil and gas plays “A” through “D” zones (fig. 2). Just over half of the Red River’s will emerge across western North Dakota. One formation that oil production has come from horizontal wells drilled within the has previously experienced “hot play” status and may be poised “B” zone of southwestern Bowman County, a prolific oil play to one day re-emerge into the spotlight of the oil and gas industry that emerged during the late 1990s and was North Dakota’s “hot is the deeply buried Red River Formation.
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • Control and Distribution of Porosity in the Red River C Laminated Member
    Control and distribution of porosity in the Red River C laminated member at the Brush Lake Field by James Roy Stimson A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences Montana State University © Copyright by James Roy Stimson (1985) Abstract: The Red River "C" cycle at the Brush Lake field consists of three distinct informal members; 1) the anhydrite member, 2) the laminated member, and 3) the burrowed member, in descending order. This cycle can be interpreted as a tidal flat deposit with the above members representing the supratidal, intertidal, and subtidal environments, respectively. The laminated member has been thoroughly dolomitized at Brush Lake and porosity values within the dolomites change rapidly. Evidence from Brush Lake reveals that the porosity distribution is primarily the result of diagenetic controls rather than structural or depositional controls. Textural evidence from the laminated member indicates that porosity has been reduced in some parts of the laminated member by 1) early precipitation of calcite cements, 2) overdolomitization, 3) early precipitation of gypsum, 4) late precipitation of replacive anhydrite, and 5) pressure solution along low amplitude stylolites. CONTROL AND DISTRIBUTION OF POROSITY IN THE RED RIVER "C" LAMINATED MEMBER AT THE BRUSH LAKE FIELD by James Roy Stimson A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences MONTANA STATE UNIVERSITY Bozeman, Montana May, 1985 St 55 Ii APPROVAL of a thesis submitted by James Roy Stimson This thesis has been read by each member of the thesis committee and has been found to be satisfactory regarding content, English usage, format, citations, bibliographic style, and consistency, and is ready for submission to the College of Graduate Studies.
    [Show full text]
  • 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).
    [Show full text]
  • Subsurface Characterisation and Geological Monitoring of the CO2 Injection Operation at Weyburn, Saskatchewan, Canada
    Subsurface characterisation and geological monitoring of the CO2 injection operation at Weyburn, Saskatchewan, Canada JAMES B. RIDING & CHRISTOPHER A. ROCHELLE British Geological Survey, Keyworth, Nottingham NG12 5GG, UK (e-mail: [email protected]; [email protected]) Abstract: The IEA Weyburn Carbon Dioxide (CO2) Monitoring and Storage Project analysed the effects of a miscible CO2 flood into a Lower Carboniferous carbonate reservoir rock at an onshore Canadian oilfield. Anthropogenic CO2 is being injected as part of a commercial enhanced oil recovery operation. Much of the research performed in Europe as part of an international monitoring project was aimed at analysing the long-term migration pathways of CO2 and the effects of CO2 on the hydrochemical and mineralogical properties of the reservoir rock. The pre-CO2 injection hydrochemical, hydrogeological and petrographical conditions in the reservoir were investigated in order to recognise changes caused by the CO2 flood and to assess the long-term fate of the injected CO2. The Lower Carboniferous (Mississippian) aquifer has a salinity gradient in the Weyburn area, where flows are oriented southwest-northeast. Hydrogeological modelling indicates that dissolved CO2 would migrate from Weyburn in an east-northeast direction at a rate of about 0.2 m/year under the influence of regional groundwater flow. The baseline gas fluxes and CO2 concentrations in groundwater were also investigated. The gas dissolved in the reservoir waters allowed potential transport pathways to be identified. Analysis of reservoir fluids proved that dissolved CO2 and methane (CH4) increased significantly in the injection area between 2002 and 2003. Most of the injected CO2 exists in a supercritical state, lesser amounts are trapped in solution and there is little apparent mineral trapping.
    [Show full text]
  • Fort Berthold Oil and Gas Plays
    FORT BERTHOLD RESERVATION List of Topics BACKGROUND Reservation Overview Production Overview GEOLOGIC OVERVIEW Geologic History Petroleum Systems Summary of Play Types CONVENTIONAL PLAY TYPES Play 1 - Folded Structure-Mississippian Carbonate Play Play 2 - Mississippian Shoreline Play Play 3 - Mississippian Lodgepole Waulsortian Mounds Play 4 - Ordovician Red River Play Play 5 - Devonian Nisku-Duperow Play Play 6 - Pre-Prairie (Winnipegosis/Interlake Play) Play 7 - Post Madison Clastics (Tyler-Heath) Play 8 - Pre-Red River Gas Play Play 9 - Bakken Fairway/Sanish Sand Play UNCONVENTIONAL / HYPOTHETICAL PLAY TYPES Play 10 - Niobrara Microbial Gas Play REFERENCES OVERVIEW there are approximately 10 formations proved to be productive in the Fort Land Status Berthold area. Of further note, the facies distribution during lower Mississippian The Fort Berthold Indian Reservation was established by the Fort Laramie FORT BERTHOLD RESERVATION Treaty of September 17, 1851, for the Arikara, Mandan, and Hidatsa Tribes of The Three Affiliated Tribes time strongly suggests that Lodgepole trends are present on the Fort Berthold Indian Reservation (USGS). Indians who later united to form the Three Affiliated Tribes. Executive Orders The Three Affiliated Tribes have purchased seismic data from lines located in and Congressional Acts have limited the reservation to its present boundaries. Tribal Headquarter: New Town, North Dakota the western portion of the Reservation, which may be examined by parties The act of June 1, 1910, 36 Stat. 455, opened unallotted and unsold reservation Geologic Setting: Williston Basin interested in oil and gas exploration. Some of the seismic data will be lands to non Indians, thus creating the "ceded and diminished lands" boundary.
    [Show full text]
  • 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.
    [Show full text]
  • Index to the Geologic Names of North America
    Index to the Geologic Names of North America GEOLOGICAL SURVEY BULLETIN 1056-B Index to the Geologic Names of North America By DRUID WILSON, GRACE C. KEROHER, and BLANCHE E. HANSEN GEOLOGIC NAMES OF NORTH AMERICA GEOLOGICAL SURVEY BULLETIN 10S6-B Geologic names arranged by age and by area containing type locality. Includes names in Greenland, the West Indies, the Pacific Island possessions of the United States, and the Trust Territory of the Pacific Islands UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.G. - Price 60 cents (paper cover) CONTENTS Page Major stratigraphic and time divisions in use by the U.S. Geological Survey._ iv Introduction______________________________________ 407 Acknowledgments. _--__ _______ _________________________________ 410 Bibliography________________________________________________ 410 Symbols___________________________________ 413 Geologic time and time-stratigraphic (time-rock) units________________ 415 Time terms of nongeographic origin_______________________-______ 415 Cenozoic_________________________________________________ 415 Pleistocene (glacial)______________________________________ 415 Cenozoic (marine)_______________________________________ 418 Eastern North America_______________________________ 418 Western North America__-__-_____----------__-----____ 419 Cenozoic (continental)___________________________________
    [Show full text]
  • Stratigraphy and Sedimentary Facies Or the Madison Limestone and Associated Rocks in Parts Pf Montana, Nebraska, North Dakota, S
    Stratigraphy/"~t * 1 and1 Sedimentaryf~^ "I * FaciesT ^ orf-» the Madison Limestone and Associated Rocks in Parts pf Montana, Nebraska, North Dakota, South Dakota, and Wyoming GEOLOGICAL SURVEY PROFESSIONAL PAPER 1273-A Stratigraphy and Sedimentary Fades of the Madison Limestone and Associated Rocks in Parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming By JAMES A. PETERSON GEOLOGY AND HYDROLOGY OF THE MADISON LIMESTONE AND ASSOCIATED ROCKS IN PARTS OF MONTANA, NEBRASKA, NORTH DAKOTA, SOUTH DAKOTA, AND WYOMING GEOLOGICAL SURVEY PROFESSIONAL PAPER 1273-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1984 DEPARTMENT OF THE INTERIOR WILLIAM P. CLARK, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Peterson, James A. Stratigraphy and sedimentary facies of the Madison Umestone and associated rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming. (Geological Survey professional paper ; 1273A) Bibliography: p. Supt. of Docs, no.: 119.16:1273-A 1. Limestone Middle West. 2. Geology, Stratigraphic Paleozoic. I. Title. II. Series. QE471.15.L5P47 1981 552'.5 82-600376 For sale by the Distribution Branch, U.S. Geological Survey, 604 South Pickett Street, Alexandria, VA 22304 CONTENTS Page Page Abstract ._.__.__.._.................._-.__.. Al Stratigraphy and sedimentary facies Continued Introduction.................................. 1 Mississippian rocks Continued Acknowledgments .............................. 2 Madison Limestone Continued Regional paleogeography and paleostructure ........... 3 M-7 to M-8.5 interval (middle Osagean) ..... A18 Stratigraphy and sedimentary facies ................. 6 M-8.5 to M-12 interval (upper Osagean) ...... 19 Precambrian rocks .......................... 6 M-12 to Me interval (approximately Cambrian rocks ....................______._ 6 Meramecian) ....................
    [Show full text]