Us Department of the Interior Us Geological Survey Open
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Baylor Geological Studies
BAYLORGEOLOGICA L STUDIES PAUL N. DOLLIVER Creative thinking is more important than elaborate FRANK PH.D. PROFESSOR OF GEOLOGY BAYLOR UNIVERSITY 1929-1934 Objectives of Geological Training at Baylor The training of a geologist in a university covers but a few years; his education continues throughout his active life. The purposes of train ing geologists at Baylor University are to provide a sound basis of understanding and to foster a truly geological point of view, both of which are essential for continued professional growth. The staff considers geology to be unique among sciences since it is primarily a field science. All geologic research in cluding that done in laboratories must be firmly supported by field observations. The student is encouraged to develop an inquiring ob jective attitude and to examine critically all geological concepts and principles. The development of a mature and professional attitude toward geology and geological research is a principal concern of the department. Frontis. Sunset over the Canadian River from near the abandoned settlement of Old Tascosa, Texas. The rampart-like cliffs on the horizon first inspired the name "Llano Estacado" (Palisaded Plain) among Coronado's men. THE BAYLOR UNIVERSITY PRESS WACO, TEXAS BAYLOR GEOLOGICAL STUDIES BULLETIN NO. 42 Cenozoic Evolution of the Canadian River Basin Paul N. DoUiver BAYLOR UNIVERSITY Department of Geology Waco, Texas Spring 1984 Baylor Geological Studies EDITORIAL STAFF Jean M. Spencer Jenness, M.S., Editor environmental and medical geology O. T. Ph.D., Advisor, Cartographic Editor what have you Peter M. Allen, Ph.D. urban and environmental geology, hydrology Harold H. Beaver, Ph.D. -
Unsolved Geological Problems in Oklahoma in 1925
136 THE UNIVERSlTY OF OKLAHOMA XXXII. UNSOLVED GEOLQGICAL PROBLEMS IN OKLAHOMA IN 1925 By eha•. N. Gould, Oklahoma Geological Survey Thirty years ago Mr. Joseph A. T~f of the. Unit.ed Statc~ Geological Survey began work'on the coal fields of Indian 'Uddea. 1. A.. The'lUaa Rock of tile HiP PIaiu. BaD. A.-oc. Pet. (ieoI.. .~oI. VII. J'23, p. 12·74. THE OKLAHOMA ACADEMY OF SCIENCE 137 Territory., Twenty-~ive yea~s,ago the writer founded the D.epart ment of Geology at the University of Oklahoma. For more thaa half the in'tervening time there were relatively few working geolo gists in Oklahoma but during the last decade the numb'er has in creased. The exact number o~ 'geologists living in Oklahoma is un known' but. there are somewhere around 300 names registerett irom this state on t,he rolls of American Association of Petroleum Geologists, and this of course does not represent the entire' nunt- I,er of geologists in the state. ', It might appear to the casual observer that300 men, :fome O'! who~ have been wor'king for at least a decade, should hav" ~olved practically all the ge'ological probiems in the state: As early as 1905, when E. G. Woodruff and I were the 'onl)' working geologists in Oklahoma, in order to attempt to outlin!: the magnftude o~ the <£ubject I prepared a list of the probleQ\ll to be solved in 'Oklahoma geology. So far as I know this list was never pu'blished and I am not now able to find it. -
Pre-Atoka Rocks of Northern Arkansas
Pre-Atoka Rocks of Northern Arkansas GEOLOGICAL SURVEY PROFESSIONAL PAPER 314-H Pre-Atoka Rocks of Northern Arkansas By SHERWOOD E. FREZON and ERNEST E. CLICK SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 314-H Thickness, lithofacies, and geologic history of potential oil and gas producing rocks of Paleozoic age in northern Arkansas UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U. S. Geological Survey Library has cataloged this publication as follows: Frezon, Sherwood Earl, 1921- Pre-Atoka rocks of northern Arkansas, by Sherwood E. Frezon and Ernest E. Glick. Washington, U. S. Govt. Print. Off., 1959. iii, 171-189 p. maps, diagrs., table. 30 cm. (U. S. Geological Sur vey. Professional paper 314-H. Shorter contributions to general geology) Part of illustrative matter fold, col., in pocket. Bibliography: p. 186-187. 1. Geology Arkansas. 2. Rocks, Sedimentary. 3. Geology, Strati- graphic Paleozoic. i. Glick, Ernest Earwood, 1922- joint author, n. Title. (Series: U. S. Geological Survey. Professional paper 314-H. Series: U. S. Geological Survey. Shorter contribu tions to general geology) 551.7209767 For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS Page Abstract .__----_ ---_-_._--._---__-_-____ 171 Stratigraphy Continued Page Introduction. ___ ___________________________________ 171 Probable latest Mississippian and early -
A Subsurface Stratigraphic Study of the Middle Atoka, Sebastian County, Arkansas Sara Beth Sutton University of Arkansas, Fayetteville
University of Arkansas, Fayetteville ScholarWorks@UARK Theses and Dissertations 8-2012 A Subsurface Stratigraphic Study of the Middle Atoka, Sebastian County, Arkansas Sara Beth Sutton University of Arkansas, Fayetteville Follow this and additional works at: http://scholarworks.uark.edu/etd Part of the Geology Commons, and the Stratigraphy Commons Recommended Citation Sutton, Sara Beth, "A Subsurface Stratigraphic Study of the Middle Atoka, Sebastian County, Arkansas" (2012). Theses and Dissertations. 477. http://scholarworks.uark.edu/etd/477 This Thesis is brought to you for free and open access by ScholarWorks@UARK. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of ScholarWorks@UARK. For more information, please contact [email protected], [email protected]. A SUBSURFACE STRATIGRAPHIC STUDY OF THE MIDDLE ATOKA, SEBASTIAN COUNTY, ARKANSAS A SUBSURFACE STRATIGRAPHIC STUDY OF THE MIDDLE ATOKA, SEBASTIAN COUNTY, ARKANSAS A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology By Sara B. Sutton University of Arkansas Bachelor of Science in Geology, 2009 August 2012 University of Arkansas ABSTRACT Raster log images were analyzed to study the subsurface stratigraphy of the Middle Atoka in the Arkoma Basin of the western portion (Sebastian County) of Arkansas. The most significant sandstone units of the Middle Atoka in this area were determined to be two generally coarsening-upward sequences in the lower portion of the formation. Based on lithologic correlations, these two units were determined to be the informally named Casey and Freiburg members of the Middle Atoka. Thickness information based on picked tops was used to create isopach maps of the units of interest. -
Gypsum Karst Speleogenesis in Barber County, Kansas of the Permian Blaine Formation Kaitlyn Gauvey Fort Hays State University, [email protected]
Fort Hays State University FHSU Scholars Repository Master's Theses Graduate School Spring 2019 Gypsum Karst Speleogenesis in Barber County, Kansas of the Permian Blaine Formation Kaitlyn Gauvey Fort Hays State University, [email protected] Follow this and additional works at: https://scholars.fhsu.edu/theses Part of the Geology Commons, and the Speleology Commons Recommended Citation Gauvey, Kaitlyn, "Gypsum Karst Speleogenesis in Barber County, Kansas of the Permian Blaine Formation" (2019). Master's Theses. 3133. https://scholars.fhsu.edu/theses/3133 This Thesis is brought to you for free and open access by the Graduate School at FHSU Scholars Repository. It has been accepted for inclusion in Master's Theses by an authorized administrator of FHSU Scholars Repository. GYPSUM KARST SPELEOGENESIS IN BARBER COUNTY, KANSAS OF THE PERMIAN BLAINE FORMATION being A Thesis Presented to the Graduate Faculty of Fort Hays State University in Partial Fulfillment of the Requirements for the Degree of Master of Science by Kaitlyn L. Gauvey B.S., Sam Houston State University Date- --=5-'/--2=-'6=-/=2-=0-.,.1.=9---- - - - This thesis for the Master of Science Degree By Kaitlyn L. Gauvey has been approved Dr. Keith Bremer, Committee Member Dr. Richard Lisichenko, Committee Member ABSTRACT Field reconnaissance examining the Permian Blaine Formation and the karst features within those rocks were conducted on two ranches in Barber County, Kansas. Karst features are developed dominantly in gypsum and include caves, sinkholes, losing streams, springs, and other surficial karst features. The Blaine Formation is known as a significant karst unit and major aquifer system in Oklahoma; however, little work has been conducted in Kansas. -
THE UNIVERSITY of Oklahœia GRADUATE COLLEGE the ATOKA FORMATION W the N Œ T H SIDE of the Mcalester BASIN a DISSERTATION SUBMI
THE UNIVERSITY OF OKlAHŒiA GRADUATE COLLEGE THE ATOKA FORMATION W THE N Œ T H SIDE OF THE McALESTER BASIN A DISSERTATION SUBMITTED TO THE ŒIADUATE FACULTY in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY BY JACK GORDON BLYTHE Norman, Oklahoma 1957 THE ATOKA FORMATION ON THE NORTH SIDE OF THE McALESTER BASIN APPROVED BY j /•) • DISSERTATION CCMMITTEE ACKNOWLEDGMENTS Dr. Carl C. Branson directed this dissertation problem. Dr. George G. Huffman, Dr. E. L. Lucas, Dr. Doris Curtis, and Dr. Reginald Harris contributed helpful advice and information. The Oklahoma Geo logical Survey employed the author as field geologist during the summer of 1954. Assistance was rendered in the field by Richard Beveridge during the month of June in 1953; and Mr. A. H. Hanson of Muskogee, Oklahoma, spent a portion of one day in the field with the author, directing his attention to several fossil localities in the Atoka for mation. Mr. Irwin Gold photographed the thin sections and the fossils, Mr. June D. King took some of the field photographs, Mr. Raymond Kune instructed the author in certain procedures of drafting, and Mr. Roy Davis and Mr. Kent Gregg assisted with much of the drafting. The author's wife, Ruth, assisted in certain phases of the field work, typed preliminary drafts of the dissertation, and continually en couraged the author during all phases of the dissertation program. Ill TABLE OF CONTENTS Page LIST OF ILLUSTRATIONS .................................... vi LIST OF MAPS xiii Chapter I . INTRODUCTION 1 II. STRATIGRAPHY 10 III. SEDIMENTATIOMAL ASPECTS AND ENVIRONMENTS OF DEPOSITION 52 IV. -
Italic Page Numbers Indicate Major References]
Index [Italic page numbers indicate major references] Abbott Formation, 411 379 Bear River Formation, 163 Abo Formation, 281, 282, 286, 302 seismicity, 22 Bear Springs Formation, 315 Absaroka Mountains, 111 Appalachian Orogen, 5, 9, 13, 28 Bearpaw cyclothem, 80 Absaroka sequence, 37, 44, 50, 186, Appalachian Plateau, 9, 427 Bearpaw Mountains, 111 191,233,251, 275, 377, 378, Appalachian Province, 28 Beartooth Mountains, 201, 203 383, 409 Appalachian Ridge, 427 Beartooth shelf, 92, 94 Absaroka thrust fault, 158, 159 Appalachian Shelf, 32 Beartooth uplift, 92, 110, 114 Acadian orogen, 403, 452 Appalachian Trough, 460 Beaver Creek thrust fault, 157 Adaville Formation, 164 Appalachian Valley, 427 Beaver Island, 366 Adirondack Mountains, 6, 433 Araby Formation, 435 Beaverhead Group, 101, 104 Admire Group, 325 Arapahoe Formation, 189 Bedford Shale, 376 Agate Creek fault, 123, 182 Arapien Shale, 71, 73, 74 Beekmantown Group, 440, 445 Alabama, 36, 427,471 Arbuckle anticline, 327, 329, 331 Belden Shale, 57, 123, 127 Alacran Mountain Formation, 283 Arbuckle Group, 186, 269 Bell Canyon Formation, 287 Alamosa Formation, 169, 170 Arbuckle Mountains, 309, 310, 312, Bell Creek oil field, Montana, 81 Alaska Bench Limestone, 93 328 Bell Ranch Formation, 72, 73 Alberta shelf, 92, 94 Arbuckle Uplift, 11, 37, 318, 324 Bell Shale, 375 Albion-Scioio oil field, Michigan, Archean rocks, 5, 49, 225 Belle Fourche River, 207 373 Archeolithoporella, 283 Belt Island complex, 97, 98 Albuquerque Basin, 111, 165, 167, Ardmore Basin, 11, 37, 307, 308, Belt Supergroup, 28, 53 168, 169 309, 317, 318, 326, 347 Bend Arch, 262, 275, 277, 290, 346, Algonquin Arch, 361 Arikaree Formation, 165, 190 347 Alibates Bed, 326 Arizona, 19, 43, 44, S3, 67. -
Basin-Centered Gas Systems of the U.S. by Marin A
Basin-Centered Gas Systems of the U.S. By Marin A. Popov,1 Vito F. Nuccio,2 Thaddeus S. Dyman,2 Timothy A. Gognat,1 Ronald C. Johnson,2 James W. Schmoker,2 Michael S. Wilson,1 and Charles Bartberger1 Columbia Basin Western Washington Sweetgrass Arch (Willamette–Puget Mid-Continent Rift Michigan Basin Sound Trough) (St. Peter Ss) Appalachian Basin (Clinton–Medina Snake River and older Fms) Hornbrook Basin Downwarp Wasatch Plateau –Modoc Plateau San Rafael Swell (Dakota Fm) Sacramento Basin Hanna Basin Great Denver Basin Basin Santa Maria Basin (Monterey Fm) Raton Basin Arkoma Park Anadarko Los Angeles Basin Chuar Basin Basin Group Basins Black Warrior Basin Colville Basin Salton Mesozoic Rift Trough Permian Basin Basins (Abo Fm) Paradox Basin (Cane Creek interval) Central Alaska Rio Grande Rift Basins (Albuquerque Basin) Gulf Coast– Travis Peak Fm– Gulf Coast– Cotton Valley Grp Austin Chalk; Eagle Fm Cook Inlet Open-File Report 01–135 Version 1.0 2001 This report is preliminary, has not been reviewed for conformity with U. S. Geological Survey editorial standards and stratigraphic nomenclature, and should not be reproduced or distributed. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U. S. Government. 1Geologic consultants on contract to the USGS 2USGS, Denver U.S. Department of the Interior U.S. Geological Survey BASIN-CENTERED GAS SYSTEMS OF THE U.S. DE-AT26-98FT40031 U.S. Department of Energy, National Energy Technology Laboratory Contractor: U.S. Geological Survey Central Region Energy Team DOE Project Chief: Bill Gwilliam USGS Project Chief: V.F. -
Oklahoma Map.Eps
U.S. DEPARTMENT OF THE INTERIOR OPEN FILE REPORT 03–247 U.S. GEOLOGICAL SURVEY Version 1.0 103° Kp 37° Jm Kds Qd Kp Kds Je Kds Kp 102° Qa To To Qd Tb Jm Qd Jm Je Toa dd 101° dd Qa Jm Qa Qa Qd Qd Kp Kds Qd Je Qd Qd Qd 100° Kp Jm Pu Qa Pu Qal Pm Kk Pr To Je Qt 99° Qal Kp Pch Kc Qd dd To Pm Pf 98° Qa Pb Psp hnw hlp hol Kds Pcc Pbi Pk 97° 96° hbv hbv hbv hhg hsl 95° 37° Kc Toa Pr To Pr To Qt Pk Pw hn hsa hsa Kc Pch hlb Qt hmh Pm hva hcc hbo Kp Pcc Pf Psp hbd hch Pr hta hto hto hlp hol Pu To Pr Pm Pr Qal To Qt Pf Qal Mkr To Pu Qd Pcc Psp hwi Qal hmh Pch Pfa Pfa ho hch hbo Mpfh hn hlb Pw hn hse To Pm Pbi hto Qa Qd Qt Qt Qt hlp Pfa Qt hv hta Qd Pm Pch Pu Qt Pdc Pmd hd hnw cu Qd ha hwi Pm Po hhg hlp Qt Pdc Pg cu Qa Qa ho hn Qal hfs Pu Pr Pb Qal hbv hsl hsa Mpfh Qt To Pw hch hnw hcc Qt hlb Qd Qd cu Qd Pu Pm Pf Pb Qal Qt hva hch hlb Pch hta hol hbo Qal hd Qa hlp To Qd hn hmh Kds Qa Pb hn Qa Pu Pcc Pdc Pmd Pf hhg Mpfh Pu Qt Mkr Qd Qa hch Qd Pcc Pr Pf Qt hlp hol To To Toa Qal Pmd Pch Pbi hsl hlb Pu Pr hd hol Qt hta hbo hsa Mpfh 103° Qa Po hwi Qt To Pbi Qal hch To Toa Qa Pu Pfa hn hnw To Qa Pcc hhg hsa hmh Kk Pdc Psp Pk Pfa ho hwi hmh Pr Qt Pr Pf hta hbd hlp 102° Qal Qal Kk Pmd hlb hse Mpfh Mkr Pb Pb hsa Pm hv Pr Psp hn Pcc Pf hv hch 101° Pfa hat Pg ha Pr hbd hcc hta hol Qt Pcc Pk Pw hwi hfs Mpfh Qt Pbi Mpfh Pf hmh Pch hva hnw Qt Qt Psp To Pf Pdc Pf Pf hwi hlb hse Pr Pbi Qt hbo hta hsl Mpfh Qal hfs Pm Pdc Qt MAP UNITS Qt hbd hch Qal Pfa hsma hv Pch hch hn Qt MDO hfs Qa Alluvium Psp Salt Plains Formation hwc Wapanucka Formation and Chickachoc Chert -
Geology of a Part of Western Texas and Southeast Ern New Mexico, with Special Reference to Salt and Potash
GEOLOGY OF A PART OF WESTERN TEXAS AND SOUTHEAST ERN NEW MEXICO, WITH SPECIAL REFERENCE TO SALT AND POTASH By H. W. HOOTS PREFACE By J. A. UDDEN : It is with great pleasure that I accept the invitation of the Director of the Geological Survey, Dr. George Otis Smith, to write a brief foreword to this report on the progress of a search for potash in which both the United States Geological Survey and the Texas Bureau of Economic Geology have cooperated for a number of years. It is a search which now appears not to have been in vain. The thought that potash must have been precipitated in the seas in which the salt beds of the Permian accumulated in America has, I presume, been in the minds of all geologists interested in the study of the Permian "Red Beds." The great extent and great thickness of these salt beds early seemed to me a sufficient reason for looking for potash in connection with any explorations of these beds in Texas. On learning, through Mr. W. E. Wrather, in 1911, of the deep boring made by the S. M. Swenson estate at Spur, in Dickens County, I made arrangements, through the generous aid of Mr: C. A. Jones, in charge of the local Swenson interests, to procure specimens of the materials penetrated. It was likewise possible, later on, to obtain a series of 14 water samples from this boring, taken at depths rang ing from 800 to 3,000 feet below the surface. These samples were obtained at a tune when the water had been standing undisturbed in the hole for two months, while no drilling had been done. -
Tectonic-Sedimentary Interplay of a Multi-Sourced, Structurally
UNDER REVIEW PREPRINT This manuscript is a preprint and has been submitted for publication to the Journal of Sedimentary Research. As of June 18, 2020, this manuscript is under review and has not been accepted for publication. The content of subsequent versions may be different from this one. Once the manuscript is formally accepted, we will add the Peer-reviewed Publication DOI, through which the final version will be available. Should you have any feedback, please contact any of the authors. We appreciate it. 1 UNDER REVIEW PREPRINT 1 TECTONIC-SEDIMENTARY INTERPLAY OF A MULTI-SOURCED, 2 STRUCTURALLY-CONFINED DEEPWATER SYSTEM IN A FORELAND BASIN 3 SETTING: THE PENNSYLVANIAN LOWER ATOKA FORMATION, 4 OUACHITA MOUNTAINS, USA 5 6 Pengfei Hou*, Lesli J. Wood, Zane R. Jobe 7 Department of Geology and Geological Engineering, Colorado School of Mines 8 1516 Illinois St, Golden, CO 80525 USA 9 * Corresponding author, Email: [email protected] 2 UNDER REVIEW PREPRINT 10 ABSTRACT 11 Submarine fans deposited in structurally complex settings record important 12 information on basin evolution and tectonic-sedimentary relationships but are often poorly 13 preserved in outcrops due to post-depositional deformation. This study integrates both new 14 field data as well as data compiled from literature to demonstrate the spatial facies variability 15 of the deep-water lower Atoka formation (Lower Pennsylvanian) that occupies a structurally 16 complex early foreland-basin setting. The lower Atoka outcrops in the Ouachita Mountains 17 and the southern Arkoma Basin in the USA are divided into three structural-depositional 18 zones: foredeep, wedge-top, and foreland. -
Structural Geometry of Thrust Faulting in the Baker Mountain and Panola Quadrangles, Southeastern Oklahoma
STRUCTURAL GEOMETRY OF THRUST FAULTING IN THE BAKER MOUNTAIN AND PANOLA QUADRANGLES, SOUTHEASTERN OKLAHOMA By JUSTIN EVANS Bachelor of Science Oklahoma State University Stillwater, Oklahoma 1995 Submitted to the Faculty of the Graduate College of the Oklahoma State University in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE July, 1997 STRUCTIJRAL GEOMETRY OF THRUST FAULTING IN THE BAKER MOUNTAIN AND PANOLA QUADRANGLES, SOUTHEASTERN OKLAHOMA Thesis Approved: Thesis Advisor ~-v.-I-- M- f h\\~ ------...~-Ml J ~~ j)umzcu C. ~ Dean ·ofGraduate College 11 ACKNOWLEDGMENTS I would like to extend my deepest thanks to my commitlee chair, Dr. Ibrahim Cemen. His advice, knowledge, and guidance have been a great help throughout this study. I would also like to thank my other committee members, Dr. Zuhair AI-Shaieb for his help and expertise as well as for the use of lab equipment to finish this study, and to Dr. Gary Stewan for advice, guidance, and editing. My thanks also go out to Jeff Ronck and Syed Mehdi for their help, and viewpoints when mine got narrow. I also want to thank Dr. Jim Pucketle for his help in everything from geology to life. Thank you so much. Thanks also to Catherine Price for help and support with the computers. Thanks to Neil Suneson for OGS well log information and for unpublished map interpretations by him, C. A. Ferguson and L. R. Hemish. Thank you Mom and Dad for your love, moral, and financial support. You always taught me to push my boundaries and look over the next horizon. Finally, and most importantly, thank you to my wife Julie.