Copyright by Berton James Seuil

Total Page:16

File Type:pdf, Size:1020Kb

Copyright by Berton James Seuil Copyright by Berton James Seuil 1956 THE UNIVERSITY OP " OKLAHOMA" “ 1 ! GRADUATE COLLEGE ORIGIN AND OCCURRENCE OF BARITE IN ARKANSAS A DISSERTATION \ SUBMITTED TO THE GRADUATE FACULTY in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY BY BERTON JAMES SCULL Norman, Oklahoma 1956 ORIGIN AND OCCURRENCE OF BARITE IN ARKANSAS APPROVED BY DISSERTATION COMMITTEE TABLE OP CONTENTS Page LIST OP T A BLES.................................. vl LIST OP ILLUSTRATIONS.................................. Vil Chapter I. INTRODUCTION............................ 1 General Statement .................... 1 Properties and Uses of Barite .............. 3 Scope of the Investigation.................. 6 Methods of Investigation.................. 7 Previous W o r k ................ o Current Work........................ 11 Geography.................................. 13 II. AREAL GEOLOGY................................ l6 General Statement ..... ................ l6 Stratigraphy................................ 17 General discussion.................. 17 Paleozoic r o c k s .................... 17 Bigfork chert .......................... 17 Polk Creek shale............ 19 Blaylock sandstone...................... 21 Missouri Mountain shale ................ 27 Arkansas novaculite . ................. 30 Stanley s h a l e ............... 37 Cretaceous rocks.................. 43 Trinity formation ................ 43 Woodbine formation.................... 46 Igneous rocks .......................... 47 Regional Structure.................... 52 General statement........................ 32 Ouachita Mountains........................ 52 Mountain systems........................ 54 Basins. .......................... 59 Athens Plateau.......................... 62 Age of the Ouachita orogeny.............. 63 iii TABLE OP CONTENTS - Continued Chapter Page Gulf Coastal P l a i n .......................... 67 Igneous structure........................... 70 Summary of Geologic Events ................... 73 III. ORIGIN, PAHAGENESISi AND AGE OF THE ARKANSAS BARITE DEPOSITS............................ 78 Character of the Barite. ................ 79 Replacement deposits . .................... 79 Vein deposits. .................... 90 Barite as cement In sediments. ....... 90 Origin and A g e ................................ 91 Replacement deposits ....................... 91 Relation to structure...................... 92 Relation to stratigraphy .......... 92 Modes of emplacement ................ 93 Chemical character ....'............ 101 Origin and age ............... 102 Paragenesls............................... 112 Cemented deposits.................. 123 Origin and emplacement .......... 123 Vein deposits. ..................... 129 Discordant v e i n s ......................... 129 Pèrldotlte area. ..................... 129 Cinnabar district....................... 129 Southeastern Oklahoma........... • . 130 Concordant veins In the Middle Arkansas novaculite.......................... 130 Regional Relations of the Barite Mineralization 131 IV. THE BARITE DEPOSITS - MINES AND PROSPECTS. 135 Magnet Cove District......................... 135 Chamberlin Creek syncllne............... 136 Reyburn Creek syncllne ........... 15I Cove Creek syncllne.................. 152 Trap Mountains............................. 154 Mazarn B a s i n ............................... 155 Mining operations........................... 155 Pigeon Roost District......................... 156 Fancy Hill District......................... 165 Gap Mountain deposit................ I60 Fancy Hill deposit................... 174 Sulphur Mountain deposit ......... 183 Dempsey Cogburn deposit................ 1Ô4 Boone Spring Creek prospect................. 185 Iv TABLE OF CONTENTS - Continued Chapter Page Polk Creek Mountain prospect ............ I85 Hatfield District.......................... 187 Bee Mountain prospect.................... 18S Boar Tusk Mountain prospects............ 188 Two Mile Creek prospects................ 191 Dierks District............................ 192 Northwest 1 6 ............................ 193 Northeast 1 6 ............................ 194 Cherry deposit .......................... 194 Lucky 13 deposit........................ 197 ! BIBLIOGRAPHY. ................................ 202 LIST OF TABLES Fable Page 1. Statistics - Arkansas Barite .......... 5 2. Section of the Blaylock Sandstone......... 23 3. Section of the Arkansas Novaculite ............ 33 4. Spectrographlc Analyses of Selected Samples from the Arkansas Barite Region. ....... 108 3. Partial Chemical Analyses of Selected Samples from the Arkansas Barite Region................ 109 vl LIST OP ILLUSTRATIONS Figure Page 1. Stratigraphie Units of the Arkansas Barite Region .................. 18 2. Sketches Depicting the Origin of the Barite. I05 3 . Geologic Map of Pigeon Roost District..........I60 4. Location Nap of Barite Lenses, Pigeon Roost District ................ 161 3 . Geologic Map of Gap Mountain Deposit ..... 172 6. Cross Section of Gap Mountain Deposit. .... 173 7 . Plan and Cross Section, Exploratory Trenches, Fancy Hill Deposit »... .................. 182 8. Geologic Map of Hatfield District..............190 9 . Sketch Map of Northeast 16 Deposit, Dierks District. ...................... 193 10. Sketch Map of Northwest I6 Deposit, Dierks District.......... I96 11. Sketch Map of Cherry Deposit, Dierks District. 199 12. Exploration Map of Lucky 13 Deposit, Dierks District. ...................... 200 Plate Page I Location Map of Districts and Deposits of the Arkansas Barite Region .......... 2 ,11 Generalized Regional Structure Map ...... 53 III Geologic Map of the Magnet Cove District .in pocket IV Cross Sections of the Magnet Cove District ...................... in pocket V Geologic Map of the Fancy Hill District, in pocket VI Cross Section F - F', Chamberlin Creek Syncline . .................... in pocket VII Cross Section E - E', Chamberlin Creek %mcline in pocket VIII Cross Section D - D ‘, Chamberlin Creek Syncline ................ in pocket DC Cross Section C - C , Chamberlin Creek Syncline ............ ..... in pocket X Geologic Map of the Chamberlin Creek Syncline Barite Deposit. in pocket vii LIST OP ILLUSTRATIONS - Continued Plate Page XI Structure Map of Mineralized Zone, Chamberlin Creek Syncline ....... in pocket XII Thickness Map of the Chamberlin Creek %mcline in pocket XIII Mine Map, Magcobar Underground Workings, Chamberlin Creek Syncline Deposit . in pocket XIV Block Diagram, Mine Workings, Chamberlin Creek Syncllne Deposit . in pocket XV Geologic Map, Western Part of Fancy Hill District ........ ..... in pocket XVI Cross Section G - G', Back Valley Syncline............ in pocket XVII Cross Section H - H*, Back Valley Syncline.................... in pocket XVIII Geologic Map of the Dierks Barite District................................ in pocket XIX Photomicrographs, Blaylock Sandstone, . 22 XX Photomicrographs, Upper Arkansas Novaculite . 32 XXI Photomicrographs of Siltstone in Stanley Formation .................. 4o XXII Photomicrographs and Photograph of Pebbly Sandstone, Stanley Formation. ........ 42 XXIII Photomicrographs, Trinity Sandstone .......... 45 XXIV (a ) Photomicrograph, Barite-Cemented I Trinity Sandstone................ 48 ! (B) Photomicrograph, Gypsum in Trinity I Formation XXV Photomicrographs, Pike G r avel............ 50 I XXVI Photomicrographs, Diamond Joe Type Syenite. 51 I XXVII Photomicrographs, Vermicular Barite Replacing Stanley Shale .................... 8l {XXVIII Photograph, Core of Nodular Barite............ 82 I XXIX Photomicrographs, Quartz Remnants in I Replacement Zone............................ 83 XXX Photomicrographs, Barite Replacing Shale, Henderson Property.......................... 84 XXXI (A) Photomicrograph, Radial Barite Rimming Clay Pellet.................... 85 (B) Photomicrograph, Barite Replacing Novaculite Pebble XXXII Photomicrographs, Zonal Development in Barite Crystals......... 86 XXXIII Photomicrographs, High-Grade Barite, Henderson Property................. 88 XXXIV Photomicrographs, High-Grade Barite, Chamberlin Creek Syncline Deposit .......... 89 viii LIST OP ILLUSTRATIONS - Contuâüëâ; Plate Page XXXy Photomicrographs« Barite-Cemented Gravel, Cherry Deposit .............. 93 XXXVI Photomicrographs, Barite-Cemented Gravel, Lucky 13 Deposit............ 94 XXXVII (A) Photomicrograph, Quartzltlc Upper Arkansas Novaculite, Chamberlin Creek Syncllne Deposit........................ 115 (B) Photomicrograph, Black Shale In Base of Stanley, Chamberlin Creek Syncllne Deposit.................. ; .......... XXXVIII Photomicrographs, Pyrite Replaced by Barite, Magnet Cove District Il6 XXXIX Photomicrographs, Replacement Sequences. • . 117 XL Photomicrographs, Barite Partially Replaced by Vein Carbonate, Magnet Cove District, . Il8 XLI (A) Photomicrograph, Differential Replacement, Mineralized Zone........................ 119 (B) Photomicrograph, "Clay" Dike, Magcobar Mine, Magnet Cove District............ XLII Photograph, Vugular Quartz Veins Cutting Stanley Shale. ............................ 120 XLIII Photograph, Crystalline Barite on Fracture Face, Magnet Cove District.................. 121 XLIV Photograph, Dense Barite Cut by Carbonate Veins, Magnet Cove District.................. 122 XLV Photomicrographs, Sandy Shale Above Mineralized Zone, Magcobar Mine. .......... 139 XLVI Photomicrographs, Altered Ouachltlte Dike, Barold Pit, Magnet Cove District............ l40 XLVII (A) Photomicrograph, Crumpled shales, Magcobar
Recommended publications
  • TEXTURES of CHERT and NOVACULITE: an EXPLORATION GUIDE Walter D
    TEXTURES OF CHERT AND NOVACULITE: AN EXPLORATION GUIDE Walter D. Keller1, Charles G. Stone2, and Alice L. Hoersch3 ABSTRACT Textures of chert and novaculite observable in scanning electron the fold belt to have attained a maximum metamorphic grade in the micrographs (SEMs) are useful as a practical, geologic ther­ zeolite to lower green schist facies. mometer for estimating the maximum temperature of those rocks Cherts and novaculites adjacent to Magnet Cove, a Cretaceous during and since deposition. Such information may be further ap­ age pluton in the eastern Ouachita Mountains of Arkansas, il­ plied during exploration for hydrocarbons (maturation or degrada­ lustrate a superposed overprinting of polygonal triple-point tex­ tion) and for metallic and nonmetallic minerals, in those and ture. It ranges from a background of about 5 //rn (talc grade) in associated rocks. chert 4500 meters from the pluton to about 45 fan (forsterite grade) from near the contact. Private drilling operations indicate that the Scanning electron micrographs of cherts and novaculites that pluton contact dips about 45 ° beneath much of the sedimentary crop out in the Ouachita Mountain fold belt of Arkansas and rock that exhibits locally anomalous crystallinity. Homogenization Oklahoma and in areas adjacent to exposed and buried intrusives temperatures of vein quartz determined by Herman Jackson and show a sequential range in textures from cryptocrystalline, George Nichols (1973, personal communication) show a gradient anhedral quartz in the nonmetamorphosed chert and novaculite to along this profile of slightly above 200° C in quartz 4500 meters coarse euhedral, polygonal triple-point quartz 60 micrometers (fjuxi) from the pluton to about 440° C near the contact.
    [Show full text]
  • Permian Basin, West Texas and Southeastern New Mexico
    Report of Investigations No. 201 Stratigraphic Analysis of the Upper Devonian Woodford Formation, Permian Basin, West Texas and Southeastern New Mexico John B. Comer* *Current address Indiana Geological Survey Bloomington, Indiana 47405 1991 Bureau of Economic Geology • W. L. Fisher, Director The University of Texas at Austin • Austin, Texas 78713-7508 Contents Abstract ..............................................................................................................................1 Introduction ..................................................................................................................... 1 Methods .............................................................................................................................3 Stratigraphy .....................................................................................................................5 Nomenclature ...................................................................................................................5 Age and Correlation ........................................................................................................6 Previous Work .................................................................................................................6 Western Outcrop Belt ......................................................................................................6 Central Texas ...................................................................................................................7 Northeastern Oklahoma
    [Show full text]
  • Data of Geochemistry
    Data of Geochemistry * Chapter T. Nondetrital Siliceous Sediments GEOLOGICAL SURVEY PROFESSIONAL PAPER 440-T Data of Geochemistry Michael Fleischer, Technical Editor Chapter T. Nondetrital Siliceous Sediments By EARLE R. CRESSMAN GEOLOGICAL SURVEY PROFESSIONAL PAPER 440-T Tabulation and discussion of chemical analyses of chert with respect to mineralogic composition, petrographic type, and geologic occurrence UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEW ART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. DATA OP GEOCHEMISTRY, SIXTH EDITION Michael Fleischer, Technical Editor The first edition of the Data of Geochemistry, by F. W. Clarke, was published in 1908 as U.S. Geological Survey Bulletin 330. Later editions, also by Clarke, were published in 1911, 1916, 1920, and 1924 as Bul­ letins 491, 616, 695, and 770. This, the sixth edition, has been written by several scientists in the Geological Survey and in other institutions in the United States and abroad, each preparing a chapter on his special field. The current edition is being published in individual chapters, titles of which are listed below. Chapters already published are indicated by boldface type. CHAPTER A. The chemical elements B. Cosmochemistry C. Internal structure and composition of the Earth D. Composition of the earth's crust E. Chemistry of the atmosphere F. Chemical composition of subsurface waters, by Donald E. White, John D. Hem, and G. A. Waring G. Chemical composition of rivers and lakes, by Daniel A. Livingstone H. Chemistry of the oceans I.
    [Show full text]
  • Mineralogical and Chemical Composition of Samples from the Christy Vanadium-Titanium Deposit, Hot Spring County, Arkansas
    UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY MINERALOGICAL AND CHEMICAL COMPOSITION OF SAMPLES FROM THE CHRISTY VANADIUM-TITANIUM DEPOSIT, HOT SPRING COUNTY, ARKANSAS By G. N. Breit1, C. Rice1, D.L. Fey2, and W.J. Sadler2 Open-File Report 92-288 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Use of trade names is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey 1 U.S. Geological Survey, Branch of Sedimentary Processes, Box 25046 MS 916 Denver Federal Center, Denver, Colorado 80225. 2 U.S. Geological Survey, Branch of Geochemistry, Box 25046 MS 973 Denver Federal Center, Denver, Colorado 80225. CONTENTS Abstract...........................................................................................! Introduction.....................................................................................! Geologic Setting.....................................................................2 Methods...........................................................................................4 Sampling..............................................................................4 Mineralogical analysis ...........................................................7 Chemical analyses.................................................................9 Whole-rock analyses.....................................................9 Partial dissolution analyses...........................................9 Statistical
    [Show full text]
  • Mapping a Novaculite Quarry in Hot Springs National Park
    Volume 2005 Article 19 2005 Mapping a Novaculite Quarry in Hot Springs National Park Mary Beth D. Trubitt Arkansas Archeological Survey, HSU Research Station, [email protected] Follow this and additional works at: https://scholarworks.sfasu.edu/ita Part of the American Material Culture Commons, Archaeological Anthropology Commons, Environmental Studies Commons, Other American Studies Commons, Other Arts and Humanities Commons, Other History of Art, Architecture, and Archaeology Commons, and the United States History Commons Tell us how this article helped you. Cite this Record Trubitt, Mary Beth D. (2005) "Mapping a Novaculite Quarry in Hot Springs National Park," Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State: Vol. 2005, Article 19. https://doi.org/ 10.21112/.ita.2005.1.19 ISSN: 2475-9333 Available at: https://scholarworks.sfasu.edu/ita/vol2005/iss1/19 This Article is brought to you for free and open access by the Center for Regional Heritage Research at SFA ScholarWorks. It has been accepted for inclusion in Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State by an authorized editor of SFA ScholarWorks. For more information, please contact [email protected]. Mapping a Novaculite Quarry in Hot Springs National Park Creative Commons License This work is licensed under a Creative Commons Attribution 4.0 License. This article is available in Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State: https://scholarworks.sfasu.edu/ita/vol2005/iss1/19 Mapping a Novaculite Quarry in Hot Springs National Park Marv Beth Trubitt, Arkansas Archeologica! Survey, Henderson State Un iversi(r Research Station, Arkadelphia, Arkansas Abstract Novaculite quarries in the Ouachita Mountains of Arkansas and Oklahoma were created through large­ scale extraction of lithic raw materials, used for stone tools by Caddos and other Native Americans over the past 11,000 years and in recent centuries by Euro-Americans for whetstones.
    [Show full text]
  • Geologic Resources Inventory Report, Hot Springs National Park
    National Park Service US Department of the Interior Natural Resource Stewardship and Science Hot Springs National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2013/741 ON THE COVER View from the top of the display spring down to the Arlington Lawn within Hot Springs National Park. THIS PAGE Gulpha Creek flows over Stanley Shale downstream from the Gulpha Gorge Campground. Photographs by Trista L. Thornberry-Ehrlich (Colorado State University) Hot Springs National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2013/741 National Park Service Geologic Resources Division PO Box 25287 Denver, CO 80225 December 2013 US Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. This report received informal peer review by subject-matter experts who were not directly involved in the collection, analysis, or reporting of the data.
    [Show full text]
  • Mineral Resources of the Caney Creek Wilderness, Polk County, Arkansas
    ~ f./ , STUDIES RELATED TO WILDERNESS · I Mineral Resources of the Caney Creek Wilderness, Polk County, Arkansas By GEORGE E. ERICKSEN and SAM H. PATTERSON U.S. GEOLOGICAL SURVEY and by MAYNARD L. DUNN, JR., and DONALD K. HARRISON, U.S. BUREAU OF MINES STUDIES RELATED TO WILDERNESS- WILDERNESS AREAS GEOLOGICAL SURVEY BULLETIN 1551 An evaluation of the mineral potential of the area UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1988 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Main entry under title: Mineral resources of the Caney Creek Wilderness, Polk County, Arkansas. (Geological Survey bulletin; 1551) Bibliography: p. Supt. of Docs. no.: I 19.3:1551 1. Mines and mineral resources-Arkansas-Caney Creek Wilderness. 2. Caney Creek Wilderness (Ark.) I. Ericksen, George Edward. II. Series. QU75.B9 no. 1551 557.3s [553'.09767'45] 83-8868 [TN 24.A7] For sale by the Distribution Branch, U.S. Geological Survey, 604 South Pickett Street, Alexandria, VA 22304 STUDIES RELATED TO WILDERNESS AREAS In accordance with the provisions of the Wilderness Act (Public Law 88-577, September 3, 1964) and the Joint Con­ ference Report on Senate Bill 4, 88th Congress, the U.S. Geological Survey and U.S. Bureau of Mines have been con- · ducting mineral surveys of wilderness and primitive areas. Studies and reports of all primitive areas have been com­ pleted. Areas officially designated as uwilderness, .. uwild," or ucanoe" when the Act was passed were incorporated into the National Wilderness Preservation System, and some of them are presently being studied.
    [Show full text]
  • Arkansas Novaculite: Whetstones and More Mary Beth Trubitt, Ph.D
    Arkansas Novaculite: Whetstones and More Mary Beth Trubitt, Ph.D. (Arkansas Archeological Survey) If you have ever used a whetstone to sharpen a knife blade, chances are it was made from Arkansas novaculite. Mining the hard rock for whetstones and sharpening stones has been an important Arkansas industry since the early 1800s. Novaculite mining for whetstone use began as early as 1818 in the Hot Springs region of the Ouachita Mountains. Initially, quantities of rock were shipped outside the state—and even outside the United States—for cutting and finishing. By the 20th century, there were local companies sawing novaculite into whetstones. Today there are at least half a dozen companies in Arkansas that manufacture and market whetstones and specialty abraders from novaculite. What is Novaculite? Novaculite is a hard, fine-grained siliceous rock, which is made up of very small crystals of the mineral quartz. It is similar to chert or flint. The name comes from the Latin word for razor. While novaculite is often white or light gray in color, it also occurs in pink, red, tan, dark gray, and black. Novaculite is distinctively translucent, and you can see light through thin edges of the rock. Geologists describe beds of massive novaculite, mixed with chert and shale, as the Arkansas Novaculite Formation. It was deposited during the Devonian to Mississippian geological periods between 318 and 416 million years ago. This rock was created when silica separated from seawater and later solidified and changed during mountain building. Folding, faulting, and tilting of rock layers has exposed novaculite on tops of mountain ridges in the Ouachita Mountains.
    [Show full text]
  • INTRODUCTION. GENERAL GEOGRAPHY and GEOLOGY of the Ridges, but Other Streams in All Parts of the Province Have Cut OUACHITA MOUNTAIN REGION
    By A. H. Pur due and H. D. Miser. INTRODUCTION. GENERAL GEOGRAPHY AND GEOLOGY OF THE ridges, but other streams in all parts of the province have cut OUACHITA MOUNTAIN REGION. their courses transverse to the ridges and thus run through LOCATION AND GENERAL RELATIONS OF THE DISTRICT. /Surface features. The Ouachita Mountain region consists of narrow, picturesque water gaps. a mountainous area known as the Ouachita Mountains and of Climate and vegetation. The climate of the region on the The area shown on the maps in this folio, which includes the Athens Plateau, which lies along the southern border of the whole is mild. The cold in winter is not extreme, but the Hot Springs and vicinity, in Arkansas, extends from latitude mountains, most of it in Arkansas. A part of the east end of the heat in summer is at times intense. The rainfall, which is 34° 22' 57" to 34° 37' 57" N. and from longitude 92° 55' 47" Ouachita Mountains is embraced in the Hot Springs district. abundant, commonly reaches a maximum in the late spring to 93° 10' 47" W. and includes one-sixteenth of a "square and early summer and decreases to a minimum late in the degree" of the earth's surface, which in that latitude amounts summer and early in the fall, when in some years there are to 245.83 square miles. It is a little southwest of the center droughts. In spite of the rather poor soil the precipitation of Arkansas, and most of it is in Garland County, but a narrow has produced a heavy forest cover over .the entire region.
    [Show full text]
  • Information Circular 39C FF-OG-OU 017
    Information Circular 39C FF-OG-OU 017 STATE OF ARKANSAS ARKANSAS GEOLOGICAL SURVEY BEKKI WHITE, DIRECTOR AND STATE GEOLOGIST INFORMATION CIRCULAR 39C STRUCTURAL AND STRATIGRAPHIC ANALYSIS OF THE SHELL INTERNATIONAL PAPER NO. 1-21 WELL, SOUTHERN OUACHITA FOLD AND THRUST BELT, HOT SPRING COUNTY, ARKANSAS Ted Godo (Shell Exploration & Production Company, Houston, TX) Peng Li (Arkansas Geological Survey, Little Rock, AR) M. Ed Ratchford (Arkansas Geological Survey, Little Rock, AR) 2014 Table of Contents List of Figures, Tables, Plates, and Appendices ................................................................ ii Acknowledgments ............................................................................................................. iii Introduction ........................................................................................................................ 1 Regional Geologic Setting ................................................................................................. 3 Stratigraphic and Structural Test Concept .................................................................... 4 Pre-Drill Reservoirs (Ordovician Sandstone Objectives) ............................................. 7 Pre-Drill Reservoirs (Bigfork Chert Objective) ............................................................ 9 Pre-Drill Structural Setting and Analysis ........................................................................ 12 Pre-Drill Thermal Maturity .............................................................................................
    [Show full text]
  • Katian GSSP and Carbonates of the Simpson and Arbuckle Groups in Oklahoma Jesse R
    University of Dayton eCommons Geology Faculty Publications Department of Geology 2015 Katian GSSP and Carbonates of the Simpson and Arbuckle Groups in Oklahoma Jesse R. Carlucci Midwestern State University Daniel Goldman University of Dayton, [email protected] Carlton E. Brett University of Cincinnati - Main Campus Stephen R. Westrop University of Oklahoma Stephen A. Leslie James Madison University Follow this and additional works at: https://ecommons.udayton.edu/geo_fac_pub Part of the Geology Commons, and the Stratigraphy Commons eCommons Citation Carlucci, Jesse R.; Goldman, Daniel; Brett, Carlton E.; Westrop, Stephen R.; and Leslie, Stephen A., "Katian GSSP and Carbonates of the Simpson and Arbuckle Groups in Oklahoma" (2015). Geology Faculty Publications. 5. https://ecommons.udayton.edu/geo_fac_pub/5 This Article is brought to you for free and open access by the Department of Geology at eCommons. It has been accepted for inclusion in Geology Faculty Publications by an authorized administrator of eCommons. For more information, please contact [email protected], [email protected]. Stratigraphy, 12 (2) 12th International Symposium on the Ordovician System Katian GSSP and Carbonates of the Simpson and Arbuckle Groups in Oklahoma Jesse R. Carlucci1 Daniel Goldman2 Carlton E. Brett3 Stephen R. Westrop4 Stephen A. Leslie5 1Assistant Professor, Kimbell School of Geosciences, Midwestern State University, Wichita Falls TX, [email protected] 2Professor & Chair, Department of Geology, University of Dayton, Dayton OH, [email protected] 3Professor, Department of Geology, University of Cincinnati, Cincinnati OH, [email protected] 4Professor & Curator of Invertebrate Paleontology, University of Oklahoma, Sam Noble Oklahoma Museum of Natural History, Norman OK, [email protected] 5Professor & Department Head, Department of Geology and Environmental Science, James Madison University, Harrisonburg VA, [email protected] 144 Stratigraphy, 12 (2) TABLE OF CONTENTS & GPS COORDINATES pg.
    [Show full text]
  • Appendix F – Minerals
    Appendix F – Minerals The Ouachita National Forest is located in Central Arkansas, within the Ouachita Mountains and the very southern portion of the Arkansas River Valley, and in southeastern Oklahoma in the Ouachita Mountains and the Red River Valley (Idabel, Oklahoma area). The geologic setting of the Forest provides a diversity of energy and non-energy mineral resources. Since approval of the 1986 Land Management Plan, minerals from the Forest, including natural gas, hardrock, and mineral materials, have been used to meet the basic needs of the public, such as providing natural gas fuel for energy sources and heating homes; stone for construction and functional home projects, and road surfacing/maintenance materials. Development of the federal and private minerals underlying the National Forest stimulates the local and national economies by making available the raw materials needed for continued economic development, resulting in increased jobs and spending. The sustainability of the Forest depends on the continued use of mineral resources to meet the public’s demand for such things as fuels and building materials. The role of mineral resources is fundamental to viability of human ecosystems. The goals for management of the Ouachita National Forest were developed in consideration of the other national forests within the Southern Region. Any decisions on projects to implement the Revised Forest Plan will be based on site-specific analysis in compliance with the National Environmental Policy Act (NEPA). These environmental analyses will be appropriately documented according to direction in the Council on Environmental Quality Regulations for Implementing the Procedural Provisions of the National Environmental Policy Act (40 CFR Parts 1500-1508) and the Environmental Policy and Procedures Handbook (FSH 1909.15).
    [Show full text]