Geomorphic Characteristics of Streams in the Mississippi
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Application of Organic Petrography in North American Shale Petroleum Systems: a Review
International Journal of Coal Geology 163 (2016) 8–51 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo Application of organic petrography in North American shale petroleum systems: A review Paul C. Hackley a, Brian J. Cardott b a U.S. Geological Survey, MS 956 National Center, 12201 Sunrise Valley Dr, Reston, VA 20192, USA b Oklahoma Geological Survey, 100 E. Boyd St., Rm. N-131, Norman, OK 73019-0628, USA article info abstract Article history: Organic petrography via incident light microscopy has broad application to shale petroleum systems, including Received 13 April 2016 delineation of thermal maturity windows and determination of organo-facies. Incident light microscopy allows Received in revised form 10 June 2016 practitioners the ability to identify various types of organic components and demonstrates that solid bitumen Accepted 13 June 2016 is the dominant organic matter occurring in shale plays of peak oil and gas window thermal maturity, whereas Available online 16 June 2016 oil-prone Type I/II kerogens have converted to hydrocarbons and are not present. High magnification SEM obser- Keywords: vation of an interconnected organic porosity occurring in the solid bitumen of thermally mature shale reservoirs Organic petrology has enabled major advances in our understanding of hydrocarbon migration and storage in shale, but suffers Thermal maturity from inability to confirm the type of organic matter present. Herein we review organic petrography applications Shale petroleum systems in the North American shale plays through discussion of incident light photographic examples. In the first part of Unconventional resources the manuscript we provide basic practical information on the measurement of organic reflectance and outline Vitrinite reflectance fluorescence microscopy and other petrographic approaches to the determination of thermal maturity. -
A Joint Local and Teleseismic Tomography Study Of
PUBLICATIONS Journal of Geophysical Research: Solid Earth RESEARCH ARTICLE A joint local and teleseismic tomography study 10.1002/2015JB012761 of the Mississippi Embayment and New Madrid Key Points: Seismic Zone • We present detailed 3-D images of Vp 1 1 1 and Vs for the upper mantle below the Cecilia A. Nyamwandha , Christine A. Powell , and Charles A. Langston ME and NMSZ • A prominent low-velocity anomaly 1Center for Earthquake Research and Information, University of Memphis, Memphis, Tennessee, USA with similar Vp and Vs anomalies is imaged in the upper mantle • Regions of similar high Vp and Vs anomalies present above and to the Abstract Detailed, upper mantle P and S wave velocity (Vp and Vs) models are developed for the northern sides of the low-velocity anomaly Mississippi Embayment (ME), a major physiographic feature in the Central United States (U.S.) and the location of the active New Madrid Seismic Zone (NMSZ). This study incorporates local earthquake and teleseismic data from the New Madrid Seismic Network, the Earthscope Transportable Array, and the Correspondence to: FlexArray Northern Embayment Lithospheric Experiment stations. The Vp and Vs solutions contain anomalies C. A. Nyamwandha, with similar magnitudes and spatial distributions. High velocities are present in the lower crust beneath the [email protected] NMSZ. A pronounced low-velocity anomaly of ~ À3%–À5% is imaged at depths of 100–250 km. High-velocity anomalies of ~ +3%–+4% are observed at depths of 80–160 km and are located along the sides and top Citation: of the low-velocity anomaly. The low-velocity anomaly is attributed to the presence of hot fluids upwelling Nyamwandha, C. -
OCTOBER 14, 2005 BLM Eastern States, Milwaukee Field Office
MISSISSIPPI NATIONAL FORESTS REASONABLE FORESEEABLE DEVELOPMENT SCENARIO FINAL REPORT: OCTOBER 14, 2005 BLM Eastern States, Milwaukee Field Office TABLE OF CONTENTS: A. Summary ....................................................................................................................................1 B. Introduction ................................................................................................................................1 C. Basis of Analysis ........................................................................................................................2 D. Description of Geology ..............................................................................................................2 E. Past and Present Fluid Mineral Exploration Activity .................................................................7 F. Past and Present Fluid Mineral Development Activity ...............................................................7 G. Future Fluid Mineral Development Potential .............................................................................8 H. Reasonable Foreseeable Development Scenario Assumptions & Discussion ............................10 I. Selected Bibliography .................................................................................................................14 J. Appendices ..................................................................................................................................15 K. Accompanying Maps .................................................................................................................15 -
On the Fundamental Difference Between Coal Rank and Coal Type
International Journal of Coal Geology 118 (2013) 58–87 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo Review article On the fundamental difference between coal rank and coal type Jennifer M.K. O'Keefe a,⁎, Achim Bechtel b,KimonChristanisc, Shifeng Dai d, William A. DiMichele e, Cortland F. Eble f,JoanS.Esterleg, Maria Mastalerz h,AnneL.Raymondi, Bruno V. Valentim j,NicolaJ.Wagnerk, Colin R. Ward l, James C. Hower m a Department of Earth and Space Sciences, Morehead State University, Morehead, KY 40351, USA b Department of Applied Geosciences and Geophysics, Montan Universität, Leoben, Austria c Department of Geology, University of Patras, 265.04 Rio-Patras, Greece d State Key Laboratory of Coal Resources and Safe Mining, China University of Mining and Technology, Beijing 100083, China e Department of Paleobiology, Smithsonian Institution, Washington, DC 20013-7012, USA f Kentucky Geological Survey, University of Kentucky, Lexington, KY 40506, USA g School of Earth Sciences, The University of Queensland, QLD 4072, Australia h Indiana Geological Survey, Indiana University, 611 North Walnut Grove, Bloomington, IN 47405-2208, USA i Department of Geology and Geophysics, College Station, TX 77843, USA j Department of Geosciences, Environment and Spatial Planning, Faculty of Sciences, University of Porto and Geology Centre of the University of Porto, Rua Campo Alegre 687, 4169-007 Porto, Portugal k School Chemical & Metallurgical Engineering, University of Witwatersrand, 2050, WITS, South Africa l School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, Australia m University of Kentucky, Center for Applied Energy Research, 2540 Research Park Drive, Lexington, KY 40511, USA article info abstract Article history: This article addresses the fundamental difference between coal rank and coal type. -
B-50 Geology of the Coastal Plain of East Central Georgia
GEORGIA STATE DIVISION OF CONSERVATION DEPARTMENT OF MINES, MINING AND GEOLOGY GARLAND PEYTON, Director THE GEOLOGICAL SURVEY BULLETIN NUMBER 50- PART 1 GEOLOGY OF THE COASTAL PLAIN OF EAST-CENTRAL GEORGIA By PHILIP E. LA MOREAUX Geologist United States Geological Survey Published in cooperation with United States Department of Interior, Geological Survey, Washing.ton, D. C. ATLANTA 1946 I LETTER OF TRANSMITTAL DEPARTMENT OF MINES, MINING AND GEOLOGY ATLANTA, February 15, 1946. His Excellency, Ellis Arnall, Governor Commissioner Ex-Officio, State Division of Conservation Through The Honorable Nelson M. Shipp, Assistant Commissioner SIR: I have the honor to submit herewith Georgia Geological Survey Bulletin No. 50, Part I, "Geology of the Coastal Plain of East-Central Georgia." This is the first in a series of bulletins under this title. Others will be published from time to time until all of the Cretaceous area in the State has been mapped. The geology of east central Georgia, the area covered in this report, influences in three essential ways the economy of the State: The Tuscaloosa formation consists of thick beds of sand and gravel that are excellent aquifers. These water-bearing beds will furnish large additional quantities of water of good quality for industrial and municipal uses throughout a belt of 10 to 30 miles in width along the northern mar gin of the Coastal Plain of Georgia. Georgia produces approximately 80 per cent of the national output of kaolin. The major portion of this production is from deposits described in this report in Washington, Wilkinson a:nd Twiggs counties. Other com mercial minerals mined in this area include bauxite, fuller's earth, lime stone, and sand and gravel. -
A Geologic Excursion to Fluorspar Mines in Hardin and Pope Counties, Illinois
Prepared for the Ninth Annual Forum on the Geology of Industrial Minerals Paducoh, Kentucky, April 27-28, 1973 A GEOLOGIC EXCURSION TO FLUORSPAR MINES IN HARDIN AND POPE COUNTIES, ILLINOIS Illinois-Kentucky Mining District and Adjacent Upper Mississippi Embayment James W. Baxter James C. Bradbury Norman C. Hester Contributions on Mine Geology D. B. Saxby B. L. Perry Illinois State Geologicol Survey Guidebook Series II A WONDERFUL AND VALUABLE FLUX. OXMXO- " FLUOR SPAR." Mined and Especially Manufactured by -^THE PEIUL MINING GOMPANY,^- ROSE CLARE, HARDIN COUNTY, ILLINOIS, For the immediate use of all Metal Workers , comprising Smelting and Refining Works, Brass and Copper Works, Car Wheel Works, Sewing Machine Works, Stove Works, Glass and Chemical Works, Agricultural Works, OR WHEREVER METAL OF ANY KIND IS SMELTED OR CASTINGS MADE. iiiiiiiiiiiiiiiiii Gentlemen : —Your close attention is earnestly invited to this new and powerful flux, endorsed by all chemists as the most searching and most favorable mineral ever discovered for the reduction and purification of metals. Our mines produce it in its purest state and without adulteration, and as it is only manufactured so as to be in the best condition for your use, we respectfully ask you to give it a trial. Kluor Spar, when exposed to heat, sends forth fumes of the most powerful fluxing, searching, purifying kind known to science, and these fumes, coming into contact with the silicates and impurities in metals, drives them out. Phosphorus and sulphur, that bllfjbear to all metals, is volatilized at once and passes off, leaving a clean, clear residue which flows without hindrance or obstruction until the last ounce of metal contained in the charge is withdrawn. -
B-127 Lithostratigraphic Framework Of
&A 'NlOO,G-3 &i flo, 12 7 g l F£i&f THE LITHOSTRATIGRAPHIC FRAMEWORK OF \;\ .-t "- THE UPPERMOST CRETACEOUS AND LOWER TERTIARY OF EASTERN BURKE COUNTY, GEORGIA Paul F. Huddlestun and Joseph H. Summerour Work Performed in Cooperation with United States Geological Survey (Cooperative Agreement Number 1434-92-A-0959) and U. S. Department of Energy (Cooperative Agreement Number DE-FG-09-92SR12868) GEORGIA DEPARTMENT OF NATURAL RESOURCES ENVIRONMENTAL PROTECTION DIVISION GEORGIA GEOLOGIC SURVEY Atlanta 1996 Bulletin 127 THE LITHOSTRATIGRAPHIC FRAMEWORK OF THE UPPERMOST CRETACEOUS AND LOWER TERTIARY OF EASTERN BURKE COUNTY, GEORGIA Paul F. Huddlestun and Joseph H. Summerour GEORGIA DEPARTMENT OF NATURAL RESOURCES Lonice C. Barrett, Commissioner ENVIRONMENTAL PROTECTION DIVISION Harold F. Reheis, Director GEORGIA GEOLOGIC SURVEY William H. McLemore, State Geologist Atlanta 1996 Bulletin 127 ABSTRACT One new formation, two new members, and a redefinition of an established lithostratigraphic unit are formally introduced here. The Oconee Group is formally recognized in the Savannah River area and four South Carolina Formations not previously used in Georgia by the Georgia Geologic Survey are recognized in eastern Burke County. The Still Branch Sand is a new formation and the two new members are the Bennock Millpond Sand Member of the Still Branch Sand and the Blue Bluff Member of the Lisbon Formation. The four South Carolina formations recognized in eastern Burke CountY include the Steel Creek Formation and Snapp Formation of the Oconee Group, the Black Mingo Formation (undifferentiated), and the Congaree Formation. The Congaree Formation and Still Branch Sand are considered to be lithostratigraphic components of the Claiborne Group. -
Water Resources of the Mississippi Embayment
Water Resources of the Mississippi Embayment GEOLOGICAL SURVEY PROFESSIONAL PAPER 448 This volume was published as separate chapters A I UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director CONTENTS [Letters designate the separately published chapters] (A) Availability of water in the Mississippi embayment, by E. M. Cushing, E. H. Boswell, P. R. Speer, R. L. Hosman, and others. (B) General geology of the Mississippi embayment, by E. M. Cushing, E. H. Boswell, and R. L. Hosman. (C) Cretaceous aquifers in the Mississippi embayment, by E. H. Boswell, G. K. Moore, L. M. MacCary, and others, with dis cussions of Quality of the water, by H. G. Jeffery. (D"» Tertiary aquifers in the Mississippi embayment, by R. L. Hosman, A. T. Long, T. W. Lambert, and others, with discussions of Quality of the water, by H. G. Jeffery. (E) Quaternary aquifers in the Mississippi embayment, by E. H. Boswell, E. M. Cushing, and R. L. Hosman, with a discussion of Quality of the water, by H. G. Jeffery. (F) Low-flow characteristics of streams in the Mississippi embayment in northern Arkansas and in Missouri, by Paul R. Speer, Marion S. Hines, M. E. Janson, and others, with a section on Quality of the water, by H. G. Jeffery. (G) Low-flow characteristics of streams in the Mississippi embayment in southern Arkansas, northern Louisiana, and north eastern Texas, by Paul R. Speer, Marion S, Hines, A. J. Calandro, and others, with a section on Quality of the water, by H. G. Jeffery. (H) Low-flow characteristics of streams in the Mississippi embayment in Tennessee, Kentucky, and Illinois, by Paul R. -
Paleoecological Analysis of the Clayton Formation (Paleocene) Near Malvern, Arkansas
The University of Southern Mississippi The Aquila Digital Community Honors Theses Honors College Spring 5-2017 Paleoecological Analysis of the Clayton Formation (Paleocene) near Malvern, Arkansas Brenna J. Hart University of Southern Mississippi Follow this and additional works at: https://aquila.usm.edu/honors_theses Part of the Paleontology Commons Recommended Citation Hart, Brenna J., "Paleoecological Analysis of the Clayton Formation (Paleocene) near Malvern, Arkansas" (2017). Honors Theses. 513. https://aquila.usm.edu/honors_theses/513 This Honors College Thesis is brought to you for free and open access by the Honors College at The Aquila Digital Community. It has been accepted for inclusion in Honors Theses by an authorized administrator of The Aquila Digital Community. For more information, please contact [email protected]. The University of Southern Mississippi Paleoecological Analysis of the Clayton Formation (Paleocene) near Malvern, Arkansas by Brenna Hart A Thesis Submitted to the Honors College of The University of Southern Mississippi in Partial Fulfillment of the Requirements for the Degree of Bachelor of Science in the Department of Geography and Geology May 2017 II Approved by ________________________________ Franklin Heitmuller, Ph.D., Associate Professor Department of Geography and Geology ________________________________ Mark Puckett, Ph.D., Chair Department of Geography and Geology ________________________________ Ellen Weinauer, Ph.D., Dean Honors College III Abstract The Clayton Formation is a section of the Midway Group immediately above the Cretaceous-Paleogene boundary that contains marine fossils from the Paleocene Epoch. The formation is composed of glauconitic sand, clay, marl, and limestone. Fossils within the formation commonly occur in clay or are concentrated in conglomeratic lag lenses. -
Slade and Paragon Formations New Stratigraphic Nomenclature for Mississippian Rocks Along the Cumberland Escarpment in Kentucky
Slade and Paragon Formations New Stratigraphic Nomenclature for Mississippian Rocks along the Cumberland Escarpment in Kentucky U.S. GEOLOGICAL SURVEY BULLETIN 1605-B Prepared in cooperation with the Kentucky Geological Survey Chapter B Slade and Paragon Formations New Stratigraphic Nomenclature for Mississippian Rocks along the Cumberland Escarpment in Kentucky By FRANK R. ETTENSOHN, CHARLES L. RICE, GARLAND R. DEVER, JR., and DONALD R. CHESNUT Prepared in cooperation with the Kentucky Geological Survey A major revision of largely Upper Mississippian nomenclature for northeastern and north-central Kentucky which includes detailed descriptions of two new formations and nine new members U.S. GEOLOGICAL SURVEY BULLETIN 1605 CONTRIBUTIONS TO STRATIGRAPHY DEPARTMENT OF THE INTERIOR WILLIAM P. CLARK, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE: 1984 For sale by Distribution Branch Text Products Section U.S. Geological Survey 604 South Pickett Street Alexandria, Virginia 22304 Library of Congress Cataloging in Publication Data Main entry under title: Slade and Paragon formations. (Contributions to stratigraphy) (U.S. Geological Survey bulletin; 1605B) Bibliography: p. Supt. of Docs, no.: I 19.3:1605-6 1. Geology, Stratigraphic Mississippian. 2. Geology Kentucky. I. Ettensohn, Frank R. II. Kentucky Geological Survey. III. Series. IV. Series: U.S. Geological Survey Bulletin ; 1605B. QE75.B9 no. 1605B 557.3 s [551.7'51] 84-600178 [QE672] CONTENTS Abstract 1 Introduction 1 Historical review -
B2150-B FRONT Final
Bedrock Geology of the Paducah 1°×2° CUSMAP Quadrangle, Illinois, Indiana, Kentucky, and Missouri By W. John Nelson THE PADUCAH CUSMAP QUADRANGLE: RESOURCE AND TOPICAL INVESTIGATIONS Martin B. Goldhaber, Project Coordinator T OF EN TH TM E U.S. GEOLOGICAL SURVEY BULLETIN 2150–B R I A N P T E E R D . I O S . R A joint study conducted in collaboration with the Illinois State Geological U Survey, the Indiana Geological Survey, the Kentucky Geological Survey, and the Missouri M 9 Division of Geology and Land Survey A 8 4 R C H 3, 1 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1998 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Mark Schaefer, Acting Director For sale by U.S. Geological Survey, Information Services Box 25286, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging-in-Publication Data Nelson, W. John Bedrock geology of the Paducah 1°×2° CUSMAP Quadrangle, Illinois, Indiana, Ken- tucky, and Missouri / by W. John Nelson. p. cm.—(U.S. Geological Survey bulletin ; 2150–B) (The Paducah CUSMAP Quadrangle, resource and topical investigations ; B) Includes bibliographical references. Supt. of Docs. no. : I 19.3:2150–B 1. Geology—Middle West. I. Title. II. Series. III. Series: The Paducah CUSMAP Quadrangle, resource and topical investigations ; B QE75.B9 no. 2150–B [QE78.7] [557.3 s—dc21 97–7724 [557.7] CIP CONTENTS Abstract .......................................................................................................................... -
Geology & Geologic History of Natchez Trace State Forest & Park
Geology & Geologic History of Natchez Trace State Forest & Park 31st Annual Central States Forest Soils Workshop TN State Geologist Frank Alexander 1952 (TN State Archives) Michael A. Gibson Dept. of Agriculture, Geosciences, & Natural Resources University of Tennessee at Martin 731.881.7435 [email protected] Geologist’s Orientation to NTSP • Geographic Scale - Regional Physiographic Setting • Stratigraphic Scale – Spans ~10 Formations • Geologic Time Scale - 400 MYA --TodayToday Regional Physiographic Setting ••NevinNevinFenneman (1938) ––PlacedPlaced in Gulf Coastal Plain ••WW TN Uplands Province – Fall Line Hills ••MaturelyMaturely dissected sand hills just west of Western Valley of TN R. Boat Ramp @ NTSP (MAG 2011) Structural “Big Picture” Setting • Part of Mississippi Embayment Synclinorum Neoproterozoic (700MYA) Rodinia Supercontinent Rifts Trench ((SubductionSubduction Rifts form Zone) (pre-Pacific) Panthalassa Ocean Spreading Rifts form the Center (pre-Atlantic) (Divergent Iapetus Ocean Zone) Orogeny (Collision Zone) Continues to exert control over many features & processes Structural “Big Picture” Setting • Same rift causing NMSZ Quakes & MS River direction • Infill from rifting of Rodinia (700 MYA ––Today)Today) Local Stratigraphic Setting & Geologic History ••NN – S trending outcrop belt • Near “Great Mz Unconformity” • Shallow dip to west • Gets Young” to west (Walther’s Law) • Oldest formations exposed (a) east & (b) lower elevations • Surface = Mostly loose K sands & clay (marine & fluvial) ••NearNear – surface Paleozoic limestone,