Database for Regional Geology, Phase 1– a Tool for Informing Regional Evaluations of Alternative Geologic Media and Decision Making
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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. -
Evaluation of the Depositional Environment of the Eagle Ford
Louisiana State University LSU Digital Commons LSU Master's Theses Graduate School 2012 Evaluation of the depositional environment of the Eagle Ford Formation using well log, seismic, and core data in the Hawkville Trough, LaSalle and McMullen counties, south Texas Zachary Paul Hendershott Louisiana State University and Agricultural and Mechanical College, [email protected] Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_theses Part of the Earth Sciences Commons Recommended Citation Hendershott, Zachary Paul, "Evaluation of the depositional environment of the Eagle Ford Formation using well log, seismic, and core data in the Hawkville Trough, LaSalle and McMullen counties, south Texas" (2012). LSU Master's Theses. 863. https://digitalcommons.lsu.edu/gradschool_theses/863 This Thesis is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Master's Theses by an authorized graduate school editor of LSU Digital Commons. For more information, please contact [email protected]. EVALUATION OF THE DEPOSITIONAL ENVIRONMENT OF THE EAGLE FORD FORMATION USING WELL LOG, SEISMIC, AND CORE DATA IN THE HAWKVILLE TROUGH, LASALLE AND MCMULLEN COUNTIES, SOUTH TEXAS A Thesis Submitted to the Graduate Faculty of the Louisiana State University Agricultural and Mechanical College in partial fulfillment of the requirements for degree of Master of Science in The Department of Geology and Geophysics by Zachary Paul Hendershott B.S., University of the South – Sewanee, 2009 December 2012 ACKNOWLEDGEMENTS I would like to thank my committee chair and advisor, Dr. Jeffrey Nunn, for his constant guidance and support during my academic career at LSU. -
Eagle Ford Group and Associated Cenomanian–Turonian Strata, U.S
U.S. Gulf Coast Petroleum Systems Project Assessment of Undiscovered Oil and Gas Resources in the Eagle Ford Group and Associated Cenomanian–Turonian Strata, U.S. Gulf Coast, Texas, 2018 Using a geology-based assessment methodology, the U.S. Geological Survey estimated undiscovered, technically recoverable mean resources of 8.5 billion barrels of oil and 66 trillion cubic feet of gas in continuous accumulations in the Upper Cretaceous Eagle Ford Group and associated Cenomanian–Turonian strata in onshore lands of the U.S. Gulf Coast region, Texas. −102° −100° −98° −96° −94° −92° −90° EXPLANATION Introduction 32° LOUISIANA Eagle Ford Marl The U.S. Geological Survey (USGS) Continuous Oil AU TEXAS assessed undiscovered, technically MISSISSIPPI Submarine Plateau-Karnes Trough Continuous Oil AU recoverable hydrocarbon resources in Cenomanian–Turonian self-sourced continuous reservoirs of 30° Mudstone Continuous Oil AU the Upper Cretaceous Eagle Ford Group Eagle Ford Marl Continuous and associated Cenomanian–Turonian Gas AU Submarine Plateau–Karnes strata, which are present in the subsurface Trough Continuous Gas AU 28° across the U.S. Gulf Coast region, Texas Cenomanian–Turonian Mudstone Continuous (fig. 1). The USGS completes geology- GULF OF MEXICO Gas AU based assessments using the elements Cenomanian–Turonian 0 100 200 MILES Downdip Continuous of the total petroleum system (TPS), 26° Gas AU 0 100 200 KILOMETERS which include source rock thickness, MEXICO NM OK AR TN GA organic richness, and thermal maturity for MS AL self-sourced continuous accumulations. Base map from U.S. Department of the Interior National Park Service TX LA FL Assessment units (AUs) within a TPS Map are defined by strata that share similar Figure 1. -
A Comparative Study of the Mississippian Barnett Shale, Fort Worth Basin, and Devonian Marcellus Shale, Appalachian Basin
DOE/NETL-2011/1478 A Comparative Study of the Mississippian Barnett Shale, Fort Worth Basin, and Devonian Marcellus Shale, Appalachian Basin U.S. DEPARTMENT OF ENERGY DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe upon privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. ACKNOWLEDGMENTS The authors greatly thank Daniel J. Soeder (U.S. Department of Energy) who kindly reviewed the manuscript. His criticisms, suggestions, and support significantly improved the content, and we are deeply grateful. Cover. Top left: The Barnett Shale exposed on the Llano uplift near San Saba, Texas. Top right: The Marcellus Shale exposed in the Valley and Ridge Province near Keyser, West Virginia. Photographs by Kathy R. Bruner, U.S. Department of Energy (USDOE), National Energy Technology Laboratory (NETL). Bottom: Horizontal Marcellus Shale well in Greene County, Pennsylvania producing gas at 10 million cubic feet per day at about 3,000 pounds per square inch. -
Chapter 4 GEOLOGY
Chapter 4 GEOLOGY CHAPTER 4 GEOLOGY ...................................................................................................................................... 4‐1 4.1 INTRODUCTION ................................................................................................................................................ 4‐2 4.2 BLACK SHALES ................................................................................................................................................. 4‐3 4.3 UTICA SHALE ................................................................................................................................................... 4‐6 4.3.2 Thermal Maturity and Fairways ...................................................................................................... 4‐14 4.3.3 Potential for Gas Production ............................................................................................................ 4‐14 4.4 MARCELLUS FORMATION ................................................................................................................................. 4‐15 4.4.1 Total Organic Carbon ....................................................................................................................... 4‐17 4.4.2 Thermal Maturity and Fairways ...................................................................................................... 4‐17 4.4.3 Potential for Gas Production ........................................................................................................... -
Stratigraphic Succession in Lower Peninsula of Michigan
STRATIGRAPHIC DOMINANT LITHOLOGY ERA PERIOD EPOCHNORTHSTAGES AMERICANBasin Margin Basin Center MEMBER FORMATIONGROUP SUCCESSION IN LOWER Quaternary Pleistocene Glacial Drift PENINSULA Cenozoic Pleistocene OF MICHIGAN Mesozoic Jurassic ?Kimmeridgian? Ionia Sandstone Late Michigan Dept. of Environmental Quality Conemaugh Grand River Formation Geological Survey Division Late Harold Fitch, State Geologist Pennsylvanian and Saginaw Formation ?Pottsville? Michigan Basin Geological Society Early GEOL IN OG S IC A A B L N Parma Sandstone S A O G C I I H E C T I Y Bayport Limestone M Meramecian Grand Rapids Group 1936 Late Michigan Formation Stratigraphic Nomenclature Project Committee: Mississippian Dr. Paul A. Catacosinos, Co-chairman Mark S. Wollensak, Co-chairman Osagian Marshall Sandstone Principal Authors: Dr. Paul A. Catacosinos Early Kinderhookian Coldwater Shale Dr. William Harrison III Robert Reynolds Sunbury Shale Dr. Dave B.Westjohn Mark S. Wollensak Berea Sandstone Chautauquan Bedford Shale 2000 Late Antrim Shale Senecan Traverse Formation Traverse Limestone Traverse Group Erian Devonian Bell Shale Dundee Limestone Middle Lucas Formation Detroit River Group Amherstburg Form. Ulsterian Sylvania Sandstone Bois Blanc Formation Garden Island Formation Early Bass Islands Dolomite Sand Salina G Unit Paleozoic Glacial Clay or Silt Late Cayugan Salina F Unit Till/Gravel Salina E Unit Salina D Unit Limestone Salina C Shale Salina Group Salina B Unit Sandy Limestone Salina A-2 Carbonate Silurian Salina A-2 Evaporite Shaley Limestone Ruff Formation -
New Insects from the Earliest Permian of Carrizo Arroyo (New Mexico, USA) Bridging the Gap Between the Carboniferous and Permian Entomofaunas
Insect Systematics & Evolution 48 (2017) 493–511 brill.com/ise New insects from the earliest Permian of Carrizo Arroyo (New Mexico, USA) bridging the gap between the Carboniferous and Permian entomofaunas Jakub Prokopa,* and Jarmila Kukalová-Peckb aDepartment of Zoology, Faculty of Science, Charles University, Viničná 7, CZ-128 43 Praha 2, Czech Republic bEntomology, Canadian Museum of Nature, Ottawa, ON, Canada K1P 6P4 *Corresponding author, e-mail: [email protected] Version of Record, published online 7 April 2017; published in print 1 November 2017 Abstract New insects are described from the early Asselian of the Bursum Formation in Carrizo Arroyo, NM, USA. Carrizoneura carpenteri gen. et sp. nov. (Syntonopteridae) demonstrates traits in hindwing venation to Lithoneura and Syntonoptera, both known from the Moscovian of Illinois. Carrizoneura represents the latest unambiguous record of Syntonopteridae. Martynovia insignis represents the earliest evidence of Mar- tynoviidae. Carrizodiaphanoptera permiana gen. et sp. nov. extends range of Diaphanopteridae previously restricted to Gzhelian. The re-examination of the type speciesDiaphanoptera munieri reveals basally coa- lesced vein MA with stem of R and RP resulting in family diagnosis emendation. Arroyohymen splendens gen. et sp. nov. (Protohymenidae) displays features in venation similar to taxa known from early and late Permian from the USA and Russia. A new palaeodictyopteran wing attributable to Carrizopteryx cf. arroyo (Calvertiellidae) provides data on fore wing venation previously unknown. Thus, all these new discoveries show close relationship between late Pennsylvanian and early Permian entomofaunas. Keywords Ephemeropterida; Diaphanopterodea; Megasecoptera; Palaeodictyoptera; gen. et sp. nov; early Asselian; wing venation Introduction The fossil record of insects from continental deposits near the Carboniferous-Permian boundary is important for correlating insect evolution with changes in climate and in plant ecosystems. -
American Armies and Battlefields in Europe 533
Chapter xv MISCELLANEOUS HE American Battle Monuments The size or type of the map illustrating Commission was created by Con- any particular operation in no way indi- Tgress in 1923. In carrying out its cates the importance of the operation; task of commeroorating the services of the clearness was the only governing factor. American forces in Europe during the The 1, 200,000 maps at the ends of W or ld W ar the Commission erected a ppro- Chapters II, III, IV and V have been priate memorials abroad, improved the placed there with the idea that while the eight military cemeteries there and in this tourist is reading the text or following the volume records the vital part American tour of a chapter he will keep the map at soldiers and sailors played in bringing the the end unfolded, available for reference. war to an early and successful conclusion. As a general rule, only the locations of Ail dates which appear in this book are headquarters of corps and divisions from inclusive. For instance, when a period which active operations were directed is stated as November 7-9 it includes more than three days are mentioned in ail three days, i. e., November 7, 8 and 9. the text. Those who desire more com- The date giYen for the relief in the plete information on the subject can find front Jine of one division by another is it in the two volumes published officially that when the command of the sector by the Historical Section, Army W ar passed to the division entering the line. -
Middle Devonian Formations in the Subsurface of Northwestern Ohio
STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Collins, Chief Report of Investigations No. 78 MIDDLE DEVONIAN FORMATIONS IN THE SUBSURFACE OF NORTHWESTERN OHIO by A. Janssens Columbus 1970 SCIENTIFIC AND TECHNICAL STAFF OF THE OHIO DIVISION OF GEOLOGICAL SURVEY ADMINISTRATIVE SECTION Horace R. Collins, State Geologist and Di v ision Chief David K. Webb, Jr., Geologist and Assistant Chief Eleanor J. Hyle, Secretary Jean S. Brown, Geologist and Editor Pauline Smyth, Geologist Betty B. Baber, Geologist REGIONAL GEOLOGY SECTION SUBSURFACE GEOLOGY SECTION Richard A. Struble, Geologist and Section Head William J. Buschman, Jr., Geologist and Section Head Richard M. Delong, Geologist Michael J. Clifford, Geologist G. William Kalb, Geochemist Adriaan J anssens, Geologist Douglas L. Kohout, Geologis t Frederick B. Safford, Geologist David A. Stith, Geologist Jam es Wooten, Geologist Aide Joel D. Vormelker, Geologist Aide Barbara J. Adams, Clerk· Typist B. Margalene Crammer, Clerk PUBLICATIONS SECTION LAKE ERIE SECTION Harold J. Fl inc, Cartographer and Section Head Charles E. Herdendorf, Geologist and Sectwn Head James A. Brown, Cartographer Lawrence L. Braidech, Geologist Donald R. Camburn, Cartovapher Walter R. Lemke, Boat Captain Philip J. Celnar, Cartographer David B. Gruet, Geologist Aide Jean J. Miller, Photocopy Composer Jean R. Ludwig, Clerk- Typist STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Collins, Chief Report of Investigations No. 78 MIDDLE DEVONIAN FORMATIONS IN THE SUBSURFACE OF NORTHWESTERN OHIO by A. Janssens Columbus 1970 GEOLOGY SERVES OHIO CONTENTS Page Introduction . 1 Previous investigations .. .. .. .. .. .. .. .. .. 1 Study methods . 4 Detroit River Group . .. .. .. ... .. ... .. .. .. .. .. .. .. ... .. 6 Sylvania Sandstone .......................... -
Geology of and Climatic Indicators in the Westphalian a New
Document generated on 09/27/2021 7:47 p.m. Atlantic Geology Geology of and climatic indicators in the Westphalian A New Glasgow formation, Nova Scotia, Canada: implications for the genesis of coal and of sandstone-hosted lead deposits F. W. Chandler Volume 34, Number 1, Spring 1998 Article abstract By the Late Carboniferous, Late Paleozoic northward drift of the continent URI: https://id.erudit.org/iderudit/ageo34_1art03 Laurentia had carried Nova Scotia from the southern dry climate belt into the equatorial rainy belt. Carboniferous amalgamation of Laurentia with the See table of contents southern continent Gondwana enclosed the area within the new supercontinent Pangea, imposing a gradually drying seasonal tropical climate. Disagreement exists on whether the early Pennsylvanian climate of the Publisher(s) Euramerican coal province was everwet or seasonal. Abundant paleopedological evidence, including calcrete-bearing vertisols, shows that Atlantic Geoscience Society during formation of Westphalian C to Stephanian coals in Nova Scotia, the climate was tropical and seasonal with a pronounced dry season, but ISSN interpretation of Westphalian A-B coal-bearing sequences lacks this form of evidence. Development of calcrete-bearing vertisols in alluvial fan deposits of 0843-5561 (print) the Westphalian A New Glasgow formation indicate that a tropical climate with 1718-7885 (digital) a pronounced dry season was already in force by early Westphalian time. During the dry season, the coal swamps of the early Westphalian Joggins and Explore this journal Springhill Mines formations were fed by groundwater from coeval alluvial fan deposits of the Polly Brook Formation at the basin margin. Sedimento-logical evidence indicates that, similarly, groundwater flowed northward from the toe Cite this article of the New Glasgow alluvial fan, but correlative palustrine sediments have not been found on land in the New Glasgow area. -
Theory and Perspective on Stimulation of Unconventional Tight
Theory and Perspective on Stimulation of Unconventional Tight Oil Reservoir in China Zhifeng Luo Professor National key Laboratory of Oil and Gas Reservoir and Exploitation; College of Oil and Gas Engineering, Southwest Petroleum University, Chengdu 610500, China; e-mail: [email protected] Yujia Gao∗ Postgraduate College of Oil and Gas Engineering, Southwest Petroleum University,Chengdu 610500, China; e-mail:[email protected] Liqiang Zhao Professor National key Laboratory of Oil and Gas Reservoir and Exploitation; College of Oil and Gas Engineering, Southwest Petroleum University,Chengdu 610500, China; e-mail: [email protected] Pingli Liu Professor National key Laboratory of Oil and Gas Reservoir and Exploitation; College of Oil and Gas Engineering, Southwest Petroleum University,Chengdu 610500, China; e-mail: [email protected] Nianyin Li Professor National key Laboratory of Oil and Gas Reservoir and Exploitation; College of Oil and Gas Engineering, Southwest Petroleum University, Chengdu 610500, China; e-mail: [email protected] ABSTRACT China has tremendous unconventional tight oil resources which are widely distributed in lots of petroliferous basin. However, compared with North American, all the tight oil reservoirs discovered in China has its own characteristics including continental sedimentation, interbeded formation, worse reservoir physical properties and less oil reserves per unit volume, which make it much harder to stimulate. Based on thorough analysis of successful stimulation experiences in North American, taking the characteristic of China’s tight oil reservoir into consideration, this article emphasized that increasing stimulated volume must be paid attention to, what’s more, integrated fracturing technology must be adopted into tight oil reservoir stimulation to promote both production and recovery efficiency.