The Appalachian-Ouachita Orogen in the United States
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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. -
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 -
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. -
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 -
West Texas Geological Society Publications and Contents Purchase from West Texas Geological Society
West Texas Geological Society Publications and Contents Purchase from West Texas Geological Society: http://www.wtgs.org/ 77-68 Geology of the Sacramento Mountains Otero County, New Mexico Regional Distribution of Phylloid Algal Mounds in Late Pennsylvanian and Wolfcampian Strata of Southern New Mexico James Lee Wilson Growth History of a Late Pennsylvanian Phylloid Algal Organic Buildup, Northern Sacramento Mains, New Mexico D.F. Toomey, J.L. Wilson, R. Rezak Paleoecological Evidence on the Origin of the Dry Canyon Pennsylvanian Bioherms James M. Parks Biohermal Submarine Cements, Laborcita Formation (Permian), Northern Sacramento Mountains, New Mexico John M. Cys and S.J. Mazzullo Carbonate and Siliciclastic Facies of the Gobbler Formation John C. Van Wagoner The Rancheria Formation: Mississippian Intracratonic Basinal Limestones Donald A. Yurewicz Stratigraphic and Structural Features of the Sacramento Mountain Escarpment, New Mexico Lloyd C. Pray Conglomeratic Lithofacies of the Laborcita and Abo Formations ( Wolfcampian), North Central Sacramento Mountains: Sedimentology and Tectonic Importance David J. Delgado Paleocaliche Textures from Wolfcampian Strata of the Sacramento Mountains, New Mexico David J. Delgado Introduction to Road Logs Lloyd C. Pray Alamogordo to Alamo Canyon and the Western Sacramento Mountains Escarpment Field Guide and Road Log “A” Lloyd C. Pray Supplemental Field Guide to Southernmost Sacramento Mountains Escarpment – Agua Chiquita and Nigger Ed Canyons Lloyd C. Pray Alamogordo to Indian Wells Reentrant Field Guide and Road Log “B” Lloyd C. Pray Guide Locality B-1-West End of Horse Ridge John C. Van Wagoner 1 Field Guide and Road Log “C” Lloyd C. Pray Plate Shaped Calcareous Algae in Late Paleozoic Rocks of Midcontinent (abstract): James M. -
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. -
South Texas Project Units 3 & 4 COLA
Rev. 08 STP 3 & 4 Final Safety Analysis Report 2.5S.1 Basic Geologic and Seismic Information The geological and seismological information presented in this section was developed from a review of previous reports prepared for the existing units, published geologic literature, interpretation of aerial photography, a subsurface investigation, and an aerial reconnaissance conducted for preparation of this STP 3 & 4 application. Previous site-specific reports reviewed include the STP 1 & 2 FSAR, Revision 13 (Reference 2.5S.1-7). A review of published geologic literature and seismologic data supplements and updates the existing geological and seismological information. A list of references used to compile the geological and seismological information presented in the following pages is provided at the end of Subsection 2.5S.1. It is intended in this section of the STP 3 & 4 FSAR to demonstrate compliance with the requirements of 10 CFR 100.23 (c). Presented in this section is information of the geological and seismological characteristics of the STP 3 & 4 site region, site vicinity, site area, and site. Subsection 2.5S.1.1 describes the geologic and tectonic characteristics of the site region and site vicinity. Subsection 2.5S.1.2 describes the geologic and tectonic characteristics of the STP 3 & 4 site area and site. The geological and seismological information was developed in accordance with NRC guidance documents RG-1.206 and RG-1.208. 2.5S.1.1 Regional Geology (200 mile radius) Using Texas Bureau of Economic Geology Terminology, this subsection discusses the physiography, geologic history, stratigraphy, and tectonic setting within a 200 mi radius of the STP 3 & 4 site. -
1 PATTERNS of MONTOYA GROUP DEPOSITION, DIAGENESIS, and RESERVOIR DEVELOPMENT in the PERMIAN BASIN Rebecca H. Jones ABSTRACT
PATTERNS OF MONTOYA GROUP DEPOSITION, DIAGENESIS, AND RESERVOIR DEVELOPMENT IN THE PERMIAN BASIN Rebecca H. Jones ABSTRACT Rocks composing both the Montoya (Upper Ordovician) and Fusselman (Lower Silurian) Formations were deposited during the global climate transition from greenhouse conditions to unusually short-lived icehouse conditions on a broad, shallow-water platform. The Montoya and the Fusselman also share many reservoir characteristics and have historically been grouped together in terms of production and plays. Recently, however, the Montoya has garnered attention on its own, with new gas production in the Permian Basin and increased interest in global Ordovician climate. Recent outcrop work has yielded new lithologic and biostratigraphic constraints and an interpretation of four third-order Montoya sequences within Sloss’s second-order Tippecanoe I sequence. The Montoya Group comprises the Upham, Aleman, and Cutter Formations, from oldest to youngest. The Upham contains a basal, irregularly present sandstone member called the Cable Canyon. The boundary between the Montoya and the Fusselman is readily definable where a thin shale called the Sylvan is present but can be difficult to discern where the Sylvan is absent. Montoya rocks were deposited from the latest Chatfieldian to the end of the Richmondian stage of the late Mohawkian and Cincinnatian series (North American) of the Upper Ordovician. Montoya reservoir quality is generally better in the northern part of the Permian Basin where it is primarily dolomite compared to limestone Montoya reservoirs in the south. Reservoir quality is also better in the lower part of the unit compared to the upper, owing to a predominance of porous and permeable subtidal ooid grainstones and skeletal packstones in the former and peritidal facies in the latter. -
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 -
Aquifers of Texas
Texas Water Development Board Report 345 Aquifers of Texas bY John B. Ashworth, Geologist and Janie Hopkins, Geologist November 1995 Aquifers of‘Texas November1935 Texas Water Development Board Craig D. Pedersen, Executive Administrator Texas Water Development Board William B. Madden, Chairman No6 Fernandez, Vice Chairman Charles W. Jenness, Member Elaine M. Barron, M.D., Member Lynwood Sanders, Member Charles L. Geren, Member Authorization for use or reproduction of any original material contained in this publication, i.e., not obtained from other sources, is freely granted. The Board would appreciate acknowledgement. Published and Distributed by the Texas Water Development Board P.O. Box 13231 Austin, Texas787 1 l-323 1 iii Aquifers of Texas November 1995 Table of Contents Page INTRODUCTION.. ................. 1 GENERAL GROUND-WATER PRINCIPLES.. 7 MAJOR AQUIFERS Ogallala. .......................... 10 Gulf Coast. ..................... 12 Edwards (Balcones Fault Zone). ..... 14 Carrizo-Wilcox. ................ 16 Trinity. ............................ 18 Edwards-Trinity (Plateau). ......... 20 Seymour. ......................... 22 Hueco-Mesilla Bolson. ..... 24 Cenozoic Pecos Alluvium. ....... 26 MINOR AQUIFERS Bone Spring-Victorio Peak. ...... 30 Dockum. ......................... 32 Brazos River Alluvium. ... 34 Hickoryv. ........................ 36 West Texas Bolsons. .......... 38 Queen City. ................. 40 Woodbine. .................. 42 Edwards-Trinity (High Plains). ... 44 Blaine. ........................ 46 Sparta. ........................ 48 Nacatoch. ...................... 50 52 lgneous. ......................... 54 Rita Blanca. .................... 56 Ellenburger-San Saba. ...... 58 Blossom. ....................... 60 Marble Falls. ................... 62 Rustler. ............................. 64 Capitan Reef Complex. .. -
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. -
Age of the Folding of the Oklahoma Mountains— % the Ouachita, Arbuckle, and Wichita Moun Tains of Oklahoma and the Llano-Burnet and Marathon Uplifts of Texas 1
BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA Vol. 39. pp. 1031-1072 December 30. 1928 AGE OF THE FOLDING OF THE OKLAHOMA MOUNTAINS— % THE OUACHITA, ARBUCKLE, AND WICHITA MOUN TAINS OF OKLAHOMA AND THE LLANO-BURNET AND MARATHON UPLIFTS OF TEXAS 1 BY SIDNEY POWERS 2 (Presented by title before the Society December SI, 1927) CONTENTS Tage Introduction ............................................................................................................. 1031 Stratigraphy ............................................................................................................. 1036 The, Ouachita Mountains ..................................................................................... 1037 Problems............................................................................................................. 1037 Age of the Carboniferous sediments .......................................................... 1038 Origin of the “glacial” boulders .................................................................. 1042 Date of the folding and overthrusting ...................................................... 1047 The Arbuckle Mountains ........................................................................................ 1049 The Wichita Mountains ........................................................................................ 1056 Former extent ................................................................................................. 1056 Criner Hills ....................................................................................................