B-87 Symposium on the Petroleum
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Subsurface Facies Analysis of the Devonian Berea Sandstone in Southeastern Ohio
SUBSURFACE FACIES ANALYSIS OF THE DEVONIAN BEREA SANDSTONE IN SOUTHEASTERN OHIO William T. Garnes A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE December 2014 Committee: James Evans, Advisor Jeffrey Snyder Charles Onasch ii ABSTRACT James Evans, Advisor The Devonian Berea Sandstone is an internally complex, heterogeneous unit that appears prominently both in outcrop and subsurface in Ohio. While the unit is clearly deltaic in outcrops in northeastern Ohio, its depositional setting is more problematic in southeastern Ohio where it is only found in the subsurface. The goal of this project was to search for evidence of a barrier island/inlet channel depositional environment for the Berea Sandstone to assess whether the Berea Sandstone was deposited under conditions in southeastern Ohio unique from northeastern Ohio. This project involved looking at cores from 5 wells: 3426 (Athens Co.), 3425 (Meigs Co.), 3253 (Athens Co.), 3252 (Athens Co.), and 3251 (Athens Co.) In cores, the Berea Sandstone ranges from 2 to 10 m (8-32 ft) thick, with an average thickness of 6.3 m (20.7 ft). Core descriptions involved hand specimens, thin section descriptions, and core photography. In addition to these 5 wells, the gamma ray logs from 13 wells were used to interpret the architecture and lithologies of the Berea Sandstone in Athens Co. and Meigs Co. as well as surrounding Vinton, Washington, and Morgan counties. Analysis from this study shows evidence of deltaic lobe progradation, abandonment, and re-working. Evidence of interdistributary bays with shallow sub-tidal environments, as well as large sand bodies, is also present. -
Ichnology, Depositional Dynamics and Sequence Stratigraphy Of
ICHNOLOGY, DEPOSITIONAL DYNAMICS AND SEQUENCE STRATIGRAPHY OF THE PLIO-PLEISTOCENE ORINOCO DELTA: MAYARO AND MORNE L’ENFER FORMATIONS, SOUTHERN TRINIDAD A Thesis Submitted to the College of Graduate Studies and Research In Partial Fulfillment of the Requirements For the Degree of Doctor of Philosophy (Ph.D.) In the Department of Geological Sciences, University of Saskatchewan, Saskatoon, Saskatchewan, Canada By SUDIPTA DASGUPTA Copyright Sudipta Dasgupta, November, 2015. All rights reserved. PERMISSION TO USE In presenting this thesis as the partial fulfillment of requirements for a Ph.D. degree from the University of Saskatchewan, I understand and confirm that the Libraries of this University may make it freely available for inspection. I agree that permission for copying of this thesis in any manner, in whole or in part, for scholarly purposes may be allowed by the Dr. Luis A. Buatois who supervised my thesis work or, in his absence, by the Head, Department of Geological Sciences, or the Dean of the Colleges of Graduate Studies and Research (CGSR), in which my thesis work was done. It is understood that any copying or publication or use of this thesis or parts thereof for any direct or indirect financial gain shall not be allowed without my written permission or, in my absence, without written permission from my immediate heir. It is also implicit that appropriate recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis. DISCLAIMER References in this thesis to any specific commercial product(s), process(es), or service(s) by trade name(s), trademark(s), manufacturer(s), private company(ies), or otherwise, does not constitute or imply its(or their) endorsement, recommendation, or favoring by me or the University of Saskatchewan. -
Geology of the Troy, Miss., 7.5 Minute Topographic Quadrangle Chickasaw and Pontotoc Counties Mississippi by Charles T
~ Geology of the Troy, Miss., 7.5 Minute Topographic Quadrangle Chickasaw and Pontotoc Counties Mississippi by Charles T. Swann, R.P.G. and Jeremy J. Dew Mississippi Mineral Resources Institute 310 Lester Hall University, Mississippi 38677 Mississippi Mineral Resources Institute Open - File Report 09-2S August, 2009 On The Cover The Mississippi Office of Geology drilled the MMRI-Reeves, No. 1 well in support of the MMRI’s surface mapping efforts. The cover picture is the drill rig set up in sand pits in sec.22, T.12S, R.3E. A set of core samples as well as a set of geophysical logs were obtained during the drilling operations. The well was begun in the lower Clayton section (Tertiary) and reached a total depth of 403 feet in the Demopolis Formation (Cretaceous). -i- TABLE OF CONTENTS On The Cover ............................................................................................................................. i Table of Contents . ..................................................................................................................... ii List of Tables ............................................................................................................................ iii List of Figures . ......................................................................................................................... iii Abstract...................................................................................................................................... 1 Introduction. ............................................................................................................................. -
Geologic Map of the Roy 7.5' Quadrangle Weber And
UTAH GEOLOGICAL SURVEY Plate 1 a divison of Utah Geological Survey Miscellaneous Publication MP-05-03 Utah Department of Natural Resources Geologic Map of the Roy 7.5' Quadrangle Qsm Qal1 Qsm Qal Qal Qal2 1 B 1 B' Qsm Qsm Qsm Qal1 Qsm Qal2 Qal2 Qsm Qsm Qal1 Qd2 Qd2 Qsm Qsm Qsm Qal1 G Qal2 Qd5 Qsm Qsm Qsm G Qal2 Qd Qdm 4 Qal2 Qd Qd1 1 Qal Qd2 Qsm 2 G Qd5 Qsm Qdm Qdm Qaf Qal3 Qd4 Qd4 Qdm Qd1 G Qd1 Qsm Qd3 Qd Qac Qdm Qdm 1 Qsm Qdm Qd5 U D Qd G Qsm Qal4 5 Qdm Qaf Qd1 Qd5 Qdm Qdm Qd1 Qac Qd Qd5 4 Qdm Qla G Qsm ? Qsm Qd Qsm 5 Qsm Qdm Qd1 Qaf Qsm Qd5 Qsm Qsm Qsm Qd5 Qdm Qsm Qda Qd4 Qd5 Qd4 G Qsm Qd Qsm 5 Qd3 Qaf Qaf Qd5 Qdm Qsm Qsm Qdm Qsm Qsm Qsm Qdm Qsm Qd5 Qsm Qd6 Qdm Qsm Qd1 Qla Qsm Qsm G Qsm Qsm Qdm Qsm Qsm Qsm Qsm Qda Qsm Qda Qd1 Qaf Qd4 Qdm U D Qsm Qd Qaf Qdm 1 G Qsm Qaf Qsm Qsm Qd6 Qaf Qdm Qsm Qaf Qaf Qd4 ? Qsm Qac Qlf G Qsm Qsm Qd3 Qat1 Qdm Qda Qaf Qaf Qd7 Qsm Qd4 Qda Qsm Qsm Qaf Qda Qat Qsm 2 Qaf Qaf Qsm Qlf G Qsm Qsm Qsm Qat3 Qaf Qac Qsm Qlf Qsm Qlf Qsm Qaf Qsm Qlf Qlf Qlf Qaf Qat Qat Qat 1 8 7 Qac G Qlf Qsm Qlf Qac Qsm Qat Qd8 5 Qat6 Qla Qal2 Qlf Qls Qaf Qlf Qd4 Qla Qac Qlf/Qd4 Qlf Qaf Qat8 Qat1 Qaf Qaf Qac Qac U D Qaf Qla Qal1 ? Qaf Qlf Qac Qaf Qlf Qat4 Qat2 Qac Qaf Qd9 Qal2 Qlf Qat Qac 3 Qaf Qaf Qd10 Qla Qla Qac Qlf Qaf Qd13 Qlf Qlf Qac Qlf/Qd G Qlf 4 Qlf Qd13 Qaf Qla Qaf Qaf Qms Qlf Qlf Qlf Qlf/Qd4 Qla Qlf/Qd4 Qla Qla Qla Qaf Qlf/Qd4 Qac Qlf Qla Qaf Qlf Qlf Qd11 Qlf Qlf Qaf Qlf/Qd4 G Qla Qla Qlf Qla Qaf Qac Qlf Qaf Qlf Qal1 Qlf Qac Qaf Qaf Qlf Qaf Qlf G Qlf Qla Qsm Qlf Qaf Qat9 Qac Qsm Qaf Qlf/Qd4 Qlf/Qd4 Qaf Qsm Qsm G Qlf Qla Qls/Qd13 Qaf Qlf Qaf Qaf Qaf Qlf Qal Qla 1 Qsm U D G Qla/Qd13 Qaf Qd12 ? Qlf/Qd4 Qls/Qd13 Qaf Qls/Qd Qla 13 Qd13 G Qla Qaf A Qlf Qd13 LH A' Base from U.S. -
CONKLIN-THESIS-2015.Pdf (7.932Mb)
QUATERNARY DEPOSITIONAL HISTORY OF A SHELF- MARGIN MINIBASIN, NORTHERN GULF OF MEXICO A Thesis Presented to the Faculty of the Department of Earth and Atmospheric Sciences University of Houston In Partial Fulfillment of the Requirements for the Degree Master of Science In Geology By Tucker Conklin May 2015 QUATERNARY DEPOSITIONAL HISTORY OF A SHELF- MARGIN MINIBASIN, NORTHERN GULF OF MEXICO ___________________________________________ Tucker Conklin APPROVED: ___________________________________________ Dr. Julia S. Wellner Chair of Committee ___________________________________________ Dr. William Sager ___________________________________________ Dr. Peter Emmet ___________________________________________ Dr. Kenneth Abdulah ___________________________________________ Dean, College of Natural Sciences and Mathematics ii Acknowledgements I would like to thank my advisor, Dr. Julia Wellner for the opportunity to work under her for my degree. I cannot thank her enough for all of the support and advice that she has given me. I would also like to thank Dr. Pete Emmet for his help in getting this project started, and for his guidance throughout the duration of my time here. I would like to extend my appreciation to Dr. William Sager, and Dr. Kenneth Abdulah (BHP Billiton) for providing excellent feedback and advice in all stages of this project. I would also like to thank my parents, Doug and Joyce Conklin, and my fiancé, Drew Barnhart for their continued support throughout these last two years. iii QUATERNARY DEPOSITIONAL HISTORY OF A SHELF- MARGIN MINIBASIN, NORTHERN GULF OF MEXICO A Thesis Presented to the Faculty of the Department of Earth and Atmospheric Sciences University of Houston In Partial Fulfillment of the Requirements for the Degree Master of Science In Geology By Tucker Conklin April 2015 iv Abstract High-resolution 3D seismic data were used to study the evolution of a shelf- margin minibasin located approximately 160 km off of the coast of Louisiana. -
Sediment Accumulation and Retention of the Changjiang (Yangtze River) Subaqueous Delta and Its Distal Muds Over the Last Century
Marine Geology 401 (2018) 2–16 Contents lists available at ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margo Sediment accumulation and retention of the Changjiang (Yangtze River) T subaqueous delta and its distal muds over the last century ⁎ Jianjun Jiaa,b, , Jianhua Gaoc, Tinglu Caib, Yan Lid, Yang Yanga, Ya Ping Wanga, Xiaoming Xiab, ⁎⁎ Jun Lie, Aijun Wangf, Shu Gaoa, a State Key Laboratory for Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China b State Research Centre for Island Exploitation and Management, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China c Ministry of Education Key Laboratory for Coast and Island Development, Nanjing University, Nanjing 210093, China d State Key Laboratory of Marine and Environmental Science, Xiamen University, Xiamen 361005, China e Qingdao Institute of Marine Geology, Qingdao 266071, China f Open Laboratory for Coast and Ocean Environmental Geology, Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, China ARTICLE INFO ABSTRACT Editor: E. Anthony Mega-deltas are major sinks of river-borne sediments and important sources of terrigenous sediments for open Keywords: shelves. Their evolution has far-reaching impacts on adjacent coastal waters, from the point of view of along- Sediment retention index shelf morphodynamics and biogeochemistry. However, the complex budgeting patterns of input, storage, bypass, Material budgeting and final accumulation of sediment are still poorly understood. The Changjiang (Yangtze River) in China is Deposition rate among the world's largest river systems, not only in terms of water and sediment discharges but also the massive Subaqueous delta amount of sediment deposited in its subaqueous delta and distal muds. -
Stratigraphy 2 2.Pdf
CONTENTS Volume 2 Number 2 2005 TEPHROSTRATIGRAPHY 101 Lindsay J. McHenry Phenocryst composition as a tool for correlating fresh and altered tephra, Bed I, Olduvai Gorge, Tanzania BIOSTRATIGRAPHY 117 T. Markham Puckett Santonian-Maastrichtian planktonic foraminiferal and ostracode biostratigraphy of the northern Gulf Coastal Plain, USA SEQUENCE STRATIGRAPHY 147 Kaiyu Liu Upper Cretaceous Sequence Stratigraphy, Sea-level Fluctuations and Oceanic Anoxic Events 2 and 3, Northeastern Gulf of Mexico CHRONOSTRATIGRAPHY 167 Markus Aretz and John Nudds The coral fauna of the Holkerian/Asbian boundary stratotype section (Carboniferous) at Little Asby Scar (Cumbria, England) and implica- tions for the boundary ICS FORUM 191 Felix M. Gradstein Definition and status of the Quaternary Phenocryst composition as a tool for correlating fresh and altered tephra, Bed I, Olduvai Gorge, Tanzania Lindsay J. McHenry *Department of Biological Sciences, Rutgers University, 610 Taylor Raod, Piscataway, New Jersey 08854 USA email: [email protected] ABSTRACT: Olduvai Gorge, Tanzania, often cited as a textbook example of continental stratigraphic study (as depicted by Hay 1976 and others) is well known for its abundant Plio-Pleistocene fauna, hominin fossils, stone artifacts, and well-dated tephra layers used widely in the calibration of human evolution. However, precise stratigraphic correlation between various sites within Olduvai has been hampered by the rarity of unaltered volcanic glass suitable for geochemical characterization. Geochemical characterization of tephra for stratigraphic correlation purposes is difficult when fresh glass is absent or secondarily altered. A multi-component approach using the major and minor element compositions of phenocrysts and glass (where present) provides successful results at Olduvai and is proposed here as a viable methodology for use elsewhere. -
Geologic Study Along Highway 45 from Tennessee Line to Meridian, Mississippi
Geologic Study Along Highway 45 From Tennessee Line to Meridian, Mississippi DONALD M. KEADY Prepared in cooperation with the Mississippi State Highway Department BULLETIN 94 MISSISSIPPI GEOLOGICAL SURVEY TRACY WALLACE LUSK Director and State Geologist UNIVERSITY, MISSISSIPPI 1962 STATE OF MISSISSIPPI Hon. Ross Robert Barnett Governor MISSISSIPPI GEOLOGICAL SURVEY BOARD Hon. Henry N. Toler, Chairman Jackson Hon. William E. Johnson, Vice Chairman Jackson Hon. D. H. Echols Jackson Hon. D. T. Keel Oxford Hon. Richard R. Priddy Jackson STAFF Tracy Wallace Lusk, M. S Director and State Geologist William Scott Parks, M. S Geologist William Halsell Moore, M. S Stratigrapher Marshall Keith Kern, B. S Geologist Margaret McCorkle Jones, M. S Secretary Elizabeth Worley Nix, B. A Librarian LETTER OF TRANSMITTAL Office of the Mississippi Geological Survey University, Mississippi June 29, 1962 Hon. Henry N. Toler, Chairman, and Members of the Geological Survey Board Gentlemen: Herewith is Mississippi Geological Survey Bulletin 94, Geologic Study Along Highway 45 From Tennessee Line to Meridian, Mississippi, by Donald M. Keady. A pressing need for prompt information along the southernmost part of this study area was the deciding factor in the selection of a highway for geologic investigation. This series of reports began in the summer of 1959 and has continued each succeeding summer—this being the third published bulletin. The author follows closely the pattern previously set, in that he describes in detail the geologic units that crop out along the route and points to specific locations for obtaining suitable topping material. He also describes the structural and geomorphic features exhibited. The writer has properly acknowledged the personnel of the Mis sissippi State Highway Department for their cooperation, nevertheless, it is fitting that these men be recognized here—Mr. -
GIS-Based Hydrogeological Platform for Sedimentary Media
[Annex I: Articles and reports related to the development of this thesis] GIS-based hydrogeological platform for sedimentary media PhD Thesis Domitila Violeta Velasco Mansilla Advisor: Dr. Enric Vázquez Suñè Hydrogeology Group (GHS) Institute of Environmental Assesment and Water Research (IDAEA), Spanish Research Council(CSIC) Dept. Geotechnical Engineering and Geosciences, Universitat Politecnica de Catalunya (UPC), Barcelona Chapter 1: Introduction I. ABSTRACT The detailed 3D hydrogeological modelling of sedimentary media (e.g. alluvial, deltaic, etc) that form important aquifers is very complex because of: (1) the natural intrinsic heterogeneity of the geological media, (2) the need for integrating reliable 3D geological models that represent this heterogeneity in the hydrogeological modelling process and (3) the scarcity of comprenhensive tools for the systematic management of spatial and temporal dependent data. The first aim of this thesis was the development of a software platform to facilitate the creation of 3D hydrogeological models in sedimentary media. It is composed of a hydrogeological geospatial database and several sets of instruments working within a GIS environment. They were designed to manage, visualise, analyse, interpret and pre and post- process the data stored in the spatial database The geospatial database (HYDOR) is based on the Personal Geodatabase structure of ArcGIS(ESRI) and enables the user to integrate into a logical and consistent structure the wide range of spatio-temporal dependent groundwater information ( e.g. geological, hydrogeological, geographical, etc data) from different sources( other database, field tests, etc) and different formats( e.g. digital data, maps etc). A set of applications in the database were established to facilitate and ensure the correct data entry in accordance with existing international standards. -
Stratigraphic Revision and Depositional Environments of the Upper Cretaceous Toreva Formation in the Northern Black Mesa Area, Navajo and Apache Counties, Arizona
Stratigraphic Revision and Depositional Environments of the Upper Cretaceous Toreva Formation in the Northern Black Mesa Area, Navajo and Apache Counties, Arizona U.S. GEOLOGICAL SURVEY BULLETIN 1685 Stratigraphic Revision and Depositional Environments of the Upper Cretaceous Toreva Formation in the Northern Black Mesa Area, Navajo and Apache Counties, Arizona By KAREN J. FRANCZYK Stratigraphic revision, sedimentology, and depositional history of Upper Cretaceous units in northern Arizona U.S. GEOLOGICAL SURVEY BULLETIN 1685 DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1988 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Franczyk, Karen J. Stratigraphic revision and depositional environments of the Upper Cretaceous Toreva Formation in the northern Black Mesa area, Navajo and Apache counties, Arizona. (U.S. Geological Survey bulletin ; 1685) Bibliography: p. 1. Toreva Formation (Ariz.) 2. Geology Stratigraphic Cretaceous. 3. Sedimentation and deposition. 4. Geology Arizona Black mesa (Navajo Coun ty and Apache County) I. Title. II. Series: Geological Survey bulletin ; 1685. QE75.B9 no. 1685a [QE688] 557.3 s 86-600212 [551.7'7'0979135] CONTENTS Abstract 1 Introduction 1 Location and acknowledgments 2 Methods of study 2 Geologic and structural setting 3 Previous work and nomenclatural history of the Toreva Formation -
Rift Basin-Fill Architecture of Fluvial-Lacustrine Lower Permian Lucaogou and Hongyanchi Low-Order Cycles, Bogda Mountains, Nw China
RIFT BASIN-FILL ARCHITECTURE OF FLUVIAL-LACUSTRINE LOWER PERMIAN LUCAOGOU AND HONGYANCHI LOW-ORDER CYCLES, BOGDA MOUNTAINS, NW CHINA A Thesis by Brad Marquis Jeffrey Bachelor of Science, University of Wisconsin – Oshkosh, 2008 Submitted to the Department of Geology and the faculty of the Graduate School of Wichita State University in partial fulfillment of the requirements for the degree of Master of Science July 2012 © Copyright 2012 by Brad Marquis Jeffrey All Rights Reserved RIFT BASIN-FILL ARCHITECTURE OF FLUVIAL-LACUSTRINE LOWER-MIDDLE PERMIAN LUCAOGOU AND HONGYANCHI FORMATIONS, NW CHINA The following faculty have examined the final copy of this thesis/dissertation for form and content, and recommend that it be accepted in partial fulfillment of the requirement for the degree of Master of Science with a major in Geology. ______________________________________ Wan Yang, Committee Chair ______________________________________ William Parcell, Committee Member ______________________________________ Collette Burke, Committee Member ______________________________________ Mary Liz Jameson, Committee Member iii ACKNOWLEDGMENTS I would like to thank my advisor, Wan Yang, for his guidance, friendship, and support. I thank the faculty and students of the Geology Department at Wichita State University for their input of ideas, interest, intriguing questions, suggestions, and discussions. I thank Qiao Feng, Yiqun Liu, Wei Li, and Neil Tabor for data and invaluable field assistance, and Wei Guan for his assistance in the field, laboratory, and international travel to the remote field area. I thank for financial support the Kansas Geological Foundation, the Graduate School of Wichita State University, Wichita State Geology Department, the Society for Sedimentary Geology, the American Association of Petroleum Geologists, and Wan Yang for his support in the field in northwestern China. -
Analysis of Lacustrine Deltaic Sedimentation in the Green River Formation, Southern Uinta Basin, Utah
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1991 Analysis of Lacustrine Deltaic Sedimentation in the Green River Formation, Southern Uinta Basin, Utah. (Volumes I and II). Robert Reginald Remy Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Remy, Robert Reginald, "Analysis of Lacustrine Deltaic Sedimentation in the Green River Formation, Southern Uinta Basin, Utah. (Volumes I and II)." (1991). LSU Historical Dissertations and Theses. 5143. https://digitalcommons.lsu.edu/gradschool_disstheses/5143 This Dissertation 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 Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps.