DOCSLIB.ORG

Mineralogical and Geochemical Analysis of Strontium and Barium Sources in the Point Pleasant Formation

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Mineralogical and Geochemical Analysis of Strontium and Barium Sources in the Point Pleasant Formation MINERALOGICAL AND GEOCHEMICAL ANALYSIS OF STRONTIUM AND BARIUM SOURCES IN THE POINT PLEASANT FORMATION Senior Research Thesis Submitted in partial fulfillment of the requirements for graduation With Research Distinction in Earth Sciences in the undergraduate colleges of The Ohio State University By Matthew Gordon Edgin The Ohio State University 2016 T ABLE OF C ONTENTS Abstract…………………………………………………………………………….ii Acknowledgements………………………………………………………………...iii List of Figures……………………………………………………………………...iv List of Tables……………………………………………………………………......v Introduction………………………………………………………………………..1 Geologic Setting………………………….………………………………………...3 Methods Leica DMS 1000 Microscope……………………...…….…………………..4 FEI Quanta 250 FEG SEM………………………….……………………...4 ICP-MS-LA……...…………..……………..……………………………….5 Data interpretation………....……………………...………………………...5 Results Leica images prior to SEM and ICP-MS-LA…..………….………………….8 SEM and EDXS………………………………………………………..…...9 Barite Estimation Calculation……………………………………...13 Induced Coupled Plasma Mass Spectrometry………………...……………14 Carbonate Shell Site A……………………………………………..15 Carbonate Shell Edge Site A……………………………………….18 Short Axis Carbonate Shell Site C………………………………….20 Bowtie Carbonate Short Axis Site D……………………………….23 Molar Sr/Ca vs Mg/Ca……………………………………………25 Discussion Barium……. …………………….………………………………………..27 Barium Mobilization……....……………………………………………….27 Strontium…………………………………………………………………28 Carbonate Crystal Structure Effects on Strontium Accommodation…...........29 Magnesium’s Influence on Strontium Incorporation into Calcite…………..30 Conclusions……………………………………………………………………….32 Recommendations for Future Work…………………………………………….…33 References Cited….……….…………………………………………………….....34 Appendices.………………….…………………………………………………....36 i A BSTRACT Analysis of trace elements in rocks from the Utica-Point Pleasant gas shale play is important because elevated concentrations of trace elements in flowback fluids derived from hydraulic fracturing may be an environmental hazard. Previous reports show high levels of barium and strontium associated with flowback fluids, with no clear explanation as to their origin. The goal of this study is to determine potential sources of Sr and Ba from Utica-Point Pleasant mudrocks that could be released into hydraulic fracturing fluids with which they interact. Polished sections of core were analyzed to determine the concentrations and distribution of trace elements across selected mineralogical/textural regions of the samples. Samples provided by Chesapeake Energy were observed with light and scanning electron microscopy (SEM) to identify areas of interest for analysis by inductively coupled plasma mass spectrometry laser ablation (ICP-MS-LA). SEM backscattered electron images and QEMSCAN mineral mapping helped determine the spatial distribution of the sulfide, sulfate, and carbonate minerals of interest. Energy dispersive spectroscopy was used to obtain semi-quantitative spot chemical analyses of minerals. SEM images show significant quantities of carbonates (CaCO3), barite (BaSO4) and celestite (SrSO4) which may be the sources of high levels of Ba and Sr in flowback fluids previously reported. Analysis from ICP-MS-LA line profiles across a pyrite/carbonate mineral assemblage and surrounding silt and clay-size carbonate/silicate matrix show major elements Mg, Ca, Sr, Ba, Al, Na, Ti, Fe, S, Si and trace elements Mo, Mn, Ni, Zn, La, Ce, U, Th, Rb. Barium concentrations were low in the pyrite and carbonate shells but ranged from 50 to 500 ppm in aluminosilicate clays in the matrix and up to 500,000 ppm in barite. Strontium concentrations ranged from 100 to 500 ppm in the pyrite but range 4000-6000 ppm in the carbonate shells and finer-grained clay-carbonate matrix. ii A CKNOWLEDGEMENTS I would like to thank the following individuals and organizations who made my entire project possible: Steve Chipera and Chesapeake Energy for providing the samples and well data for this study, everyone associated with the Subsurface Energy Materials Characterization and Analysis Lab (SEMCAL), Dr. Dave Cole, Dr. Julie Sheets, Dr. Susan Welch, Alex Swift, Derek Foley, and Edwin Buchwalter for use of their facilities, knowledge, guidance, and collaboration. I would also like to thank Dr. John Olesik for his expertise and guidance with inductive coupled plasma mass spectrometry laser ablation (ICP-MS-LA). Appreciation goes to the entire faculty, students, and staff of The Ohio State University’s School of Earth Sciences for being a truly special place to spend time pursuing my second bachelor’s degree. I would like to thank all the professors that have imparted their knowledge in the classes I have taken and contributed to my overall understanding of the Earth Sciences: Dr. Panero, Dr. Barton, Dr. Krissek, Dr. Cox, Dr. Royce, Dr. Lyons, Dr. Cook, Dr. Carey, Dr. Wilkins, Dr. Wilson, and Dale Gnidovec. I also would like to thank the School of Earth Sciences for maintaining their Field Geology program. Particularly, I want to thank Dr. Kelley, Dr. Wilson, Dr. Judge, Dr. Millan, and Dr. Darrah, the states of Utah & Nevada, and my TA’s Trish Hall & Will Blocher for their hard work, time, and commitment. Likewise, I would like to recognize my roommates Alex Grady, Sam Perry, and Murvin Morrow for making field camp one of the best experiences in my life. In addition, I would like to thank Mario Gutierrez, John Daniele, Lienne Sethna, Drew Sabula, Laura Miller, Abbie Bowman, Megan Mave, Ken Peterman, and Myles Moore for satiating all the great clichés about geologists. Special thanks to my undergraduate advisor, Dr. Anne Carey for her help, support, and patience. The utmost appreciation goes to my research advisor, Dr. Dave Cole, for his wealth of knowledge, top-notch facilities, and advice. Lastly, I would like to thank my parents and the rest of my family for being incredibly supportive of my decision to pursue a second bachelor’s degree. iii L IST OF F IGURES 1. Leica Images……………………………………………………………………………...8-9 2. SEM Images…………………………………………………………………………...10-11 3. Laser Ablation Graphs………………………………………………………………....15-25 4. Laser Ablation Site E SEM images..…………………………………………………....36-38 5. Laser Ablation Site E Graphs………………………………………………………….86-87 iv L IST OF T ABLES 1. Chesapeake Mineralogical and Petrophysical Data……………………………..…………...7 2. EDX Carbonate Analysis………………………………………………………………….12 3. Barite Estimation Calculation……………………………………………………………...13 4. Calculations of barium in bulk mineralogy…………………………...……………………27 5. Sr/Ca ratios relation with Kd……………………………………………………………...29 6. Laser ablation raw data………………………………………………………………...39-85 v I NTRODUCTION Since the shale gas boom began, there has been immense concern about the fluids and chemicals associated with hydraulic fracturing. Flowback water is defined as water that has returned to the surface when pressure is released on a hydraulically fractured well. Most of the flowback water returns to the surface within the first few days to weeks after the wells are hydraulically fractured. The remainder of the returns overtime during the production phase, when hydrocarbons are extracted from the wellsite. The water quality of the flowback waters can be affected by the chemistry of fluids in contact with the formation, fluids within the formation water, the formation itself, the amount of time the fluid was retained in the well, and the initial quality of the fluids used in the process (Vazquez et al., 2014). Although the interactions with dissolved substances in the subsurface is still being studied, it is important to note that when flowback waters return to the surface, an immense amount of water-rock interaction has taken place. These interactions have the potential to mobilize many different types of chemical compounds, which is why understanding the trace element composition of the Utica/Point Pleasant formation is important. Monitoring of trace element concentrations has been used to assess the potential environmental impact of flowback water and design strategies for how to process and dispose of the fluids. Trace elements are defined as elements with concentrations less than 0.1% in the Earth's crust (Harris et al., 2013). They are utilized to identify associations among trace elements themselves, and to identify paleoceanographic conditions and depositional processes (Harris et al., 2013). They can also be used to investigate the composition of the fluids associated with gas shale systems and detect substances potentially harmful to human health and the environment. The trace element composition of the Utica/Point Pleasant formations are of particular interest because these organic carbon rich formations are a major source of hydrocarbons. Previous studies have examined flowback waters to measure trace elements compositions and have shown high concentrations of total dissolved salts (TDS), Cl, Br, Na, Ca, Sr, Ba, Ra, and other elements. The levels of TDS, Cl and other elements are as much as 5-10 times the concentration of seawater (Haluszczak et al., 2013). Concentrations of 226Ra, 228Ra, and Ba have been found to be significantly higher than what is allowed for drinking water limits (Haluszczak et al., 2013). Flowback waters from wellsites located in or near the Appalachian Basin have been shown to contain elevated levels of barium and strontium levels as high as 3g/L (Rozell and Reaven, 2012). The levels deviate from normal water near wellsites which have Sr/Ca ratios of about 1/100 mg/L and Sr/Mg ratios of about 1/50 mg/L for water (Rozell and Reaven, 2012). Barium in high concentrations
Load more

Recommended publications
  • The Classic Upper Ordovician Stratigraphy and Paleontology of the Eastern Cincinnati Arch
    International Geoscience Programme Project 653 Third Annual Meeting - Athens, Ohio, USA Field Trip Guidebook THE CLASSIC UPPER ORDOVICIAN STRATIGRAPHY AND PALEONTOLOGY OF THE EASTERN CINCINNATI ARCH Carlton E. Brett – Kyle R. Hartshorn – Allison L. Young – Cameron E. Schwalbach – Alycia L. Stigall International Geoscience Programme (IGCP) Project 653 Third Annual Meeting - 2018 - Athens, Ohio, USA Field Trip Guidebook THE CLASSIC UPPER ORDOVICIAN STRATIGRAPHY AND PALEONTOLOGY OF THE EASTERN CINCINNATI ARCH Carlton E. Brett Department of Geology, University of Cincinnati, 2624 Clifton Avenue, Cincinnati, Ohio 45221, USA ([email protected]) Kyle R. Hartshorn Dry Dredgers, 6473 Jayfield Drive, Hamilton, Ohio 45011, USA ([email protected]) Allison L. Young Department of Geology, University of Cincinnati, 2624 Clifton Avenue, Cincinnati, Ohio 45221, USA ([email protected]) Cameron E. Schwalbach 1099 Clough Pike, Batavia, OH 45103, USA ([email protected]) Alycia L. Stigall Department of Geological Sciences and OHIO Center for Ecology and Evolutionary Studies, Ohio University, 316 Clippinger Lab, Athens, Ohio 45701, USA ([email protected]) ACKNOWLEDGMENTS We extend our thanks to the many colleagues and students who have aided us in our field work, discussions, and publications, including Chris Aucoin, Ben Dattilo, Brad Deline, Rebecca Freeman, Steve Holland, T.J. Malgieri, Pat McLaughlin, Charles Mitchell, Tim Paton, Alex Ries, Tom Schramm, and James Thomka. No less gratitude goes to the many local collectors, amateurs in name only: Jack Kallmeyer, Tom Bantel, Don Bissett, Dan Cooper, Stephen Felton, Ron Fine, Rich Fuchs, Bill Heimbrock, Jerry Rush, and dozens of other Dry Dredgers. We are also grateful to David Meyer and Arnie Miller for insightful discussions of the Cincinnatian, and to Richard A.
    [Show full text]
  • Ordovician Point Pleasant/Utica-Lower Paleozoic
    Ordovician Point Pleasant/Utica-Lower Paleozoic Total Petroleum System—Revisions to the Utica- Lower Paleozoic Total Petroleum System in the Appalachian Basin Province Scientific Investigations Report 2019–5025 U.S. Department of the Interior U.S. Geological Survey Cover. An outcrop of planar- to irregular-bedded limestone and shale of the Point Pleasant Formation that is exposed along Big Run in Clermont County, Ohio. The red and white measuring stick is approximately 0.5 meters in length (1.6 feet). Permission was required prior to entering private property to visit this exposure. Photograph from Schumacher and others (2013). Inset photograph. Well core no. 3003 (API no. 3403122838) from the Point Pleasant Formation, Coshocton County, Ohio (interval depth, 5,660–5,670 feet). Total length of core shown is approximately 3 feet. Photograph provided by Michael Solis, Ohio Department of Natural Resources, Division of Geological Survey. Ordovician Point Pleasant/Utica-Lower Paleozoic Total Petroleum System— Revisions to the Utica-Lower Paleozoic Total Petroleum System in the Appalachian Basin Province By Catherine B. Enomoto, Michael H. Trippi, and Debra K. Higley Scientific Investigations Report 2019–5025 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DAVID BERNHARDT, Secretary U.S. Geological Survey James F. Reilly II, Director U.S. Geological Survey, Reston, Virginia: 2019 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit https://www.usgs.gov or call 1–888–ASK–USGS (1–888–275–8747). For an overview of USGS information products, including maps, imagery, and publications, visit https://store.usgs.gov.
    [Show full text]
  • Ordovician News 2005
    ORDOVICIAN NEWS SUBCOMMISSION ON ORDOVICIAN STRATIGRAPHY INTERNATIONAL COMMISSION ON STRATIGRAPHY Nº 22 2005 ORDOVICIAN NEWS Nº 22 INTERNATIONAL UNION OF GEOLOGIAL SCIENCES President: ZHANG HONGREN (China) Vice-President: S. HALDORSEN (Norway) Secretary General: P. T. BOBROWSKI (Canada) Treasurer: A. BRAMBATI (Italy) Past-President: E.F.J. DE MULDER (The Netherlands) INTERNATIONAL COMMISSION ON STRATIGRAPHY Chairman: F. GRADSTEIN (Norway) Vice-Chairman: S. C. FINNEY (USA) Secretary General: J. OGG (USA) Past-Chairman: J. REMANE (Switzerland) INTERNATIONAL SUBCOMMISSION ON ORDOVICIAN STRATIGRAPHY Chairman: CHEN XU (China) Vice-Chairman: J. C. GUTIÉRREZ MARCO (Spain) Secretary: G. L. ALBANESI (Argentina) F. G. ACEÑOLAZA (Argentina) A. V. DRONOV (Russia) O. FATKA (Czech Republic) S. C. FINNEY (USA) R. A. FORTEY (UK) D. A. HARPER (Denmark) W. D. HUFF (USA) LI JUN (China) C. E. MITCHELL (USA) R. S. NICOLL (Australia) G. S. NOWLAN (Canada) A. W. OWEN (UK) F. PARIS (France) I. PERCIVAL (Australia) L. E. POPOV (Russia) M. R. SALTZMAN (USA) Copyright © IUGS 2005 i ORDOVICIAN NEWS Nº 22 CONTENTS Page NOTE FOR CONTRIBUTORS iii EDITOR'S NOTE iii CHAIRMAN´S AND SECRETARY´S ADDRESSES iii CHAIRMAN´S REPORT 1 SOS ANNUAL REPORT FOR 2001 1 INTERNATIONAL SYMPOSIA AND CONFERENCES 4 PROJECTS 7 SCIENTIFIC REPORTS 7 HONORARY NOTES 8 MISCELLANEA 9 CURRENT RESEARCH 9 RECENT ORDOVICIAN PUBLICATIONS 25 NAMES AND ADDRESS CHANGES 40 URL: http://www.ordovician.cn, http://seis.natsci.csulb.edu/ISOS Cover: The Wangjiawan GSSP for the base of the Hirnantian Stage, China. ii ORDOVICIAN NEWS Nº 22 NOTE FOR CONTRIBUTORS The continued health and survival of Ordovician News depends on YOU to send in items of Ordovician interest such as lists and reviews of recent publications, brief summaries of current research, notices of relevant local, national and international meetings, etc.
    [Show full text]
  • Business Development Opportunities in the Utica Shale Play in Consideration of the Geographic Alignment of the Fairway
    Business Development Opportunities in the Utica Shale Play in Consideration of the Geographic Alignment of the Fairway Defining Business Opportunities within a Geographic Footprint Jim Scherrer, Energy Resources Director Geologic Analysis November 2015 The purpose of this document is to highlight the current business development opportunities that arise across the breadth of the Utica Shale fairway. The oil and gas resources underlying the Marcellus from within the “Utica Shale” play have become better defined through the shale resource exploration and recovery operations of various exploration and production (E&P) Above: The “tiramisu model” companies. The geographic alignment is unique and now is provides a visualization of the better defined; offering opportunities for business horizontal drilling taking place in development that aligns with the geography of the fairway. shale repositories worldwide. Additionally, boundaries such as the “Line of Death” for economic quantities of oil and gas within the play have been better delineated. More recent test drilling within the Appalachian Basin below the Marcellus (Devonian Period), in stratigraphy generally known as the “Utica” (Ordovician Period), there has been a resurgence of activity as this carbon-rich play has yielded unexpected, very positive results. This Utica formation assessment also includes the Point Pleasant formation. Taury Smith (NY State Geological Survey) says the Utica Shale play is more appropriately called the “Utica Shale and associated organic‐rich calcareous shale and interbedded limestone and shale play.” This report relies on many sources, but primarily the Utica Shale Appalachian Basin Exploration Consortium (the Consortium). The 15 members of the Consortium were joined by individuals from four state geological surveys, two universities, one consulting company, the U.S.
    [Show full text]
  • Utica Shale Play Geology Review
    Utica Shale Play Geology review April 2017 Independent Statistics & Analysis U.S. Department of Energy www.eia.gov Washington, DC 20585 This report was prepared by the U.S. Energy Information Administration (EIA), the statistical and analytical agency within the U.S. Department of Energy. By law, EIA’s data, analyses, and forecasts are independent of approval by any other officer or employee of the United States Government. The views in this report therefore should not be construed as representing those of the U.S. Department of Energy or other federal agencies EIA author contact: Dr. Olga Popova Email: [email protected] U.S. Energy Information Administration | Utica Shale Play i April 2017 Introduction The U.S. Energy Information Administration (EIA) is adding and updating geologic information and maps of the major tight formations and shale plays for the continental United States. This document outlines updated information and maps for the Utica shale play of the Appalachian basin. The geologic features characterized include a contoured elevation of the formation top (structure), contoured thickness (isopach), paleogeography elements, and tectonic structures (regional faults and folds, etc.), as well as play boundaries, well location, and initial GOR (gas-to-oil ratio) of wells producing from January 2004 through December 2016. EIA integrates these geologic elements into a series of maps. The Utica play map consists of layers of geologic and production information that users can view either as separate thematic maps (such as Figure 1) or as interactive layers of the U.S. Energy Mapping System. Additional map layers may be added if additional geologic data (such as petrophysical and thermodynamic formation properties) become available.
    [Show full text]
  • The Depositional History of the Point Pleasant Member of the Cynthiana Formation in Northern Kentucky
    Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 12-1984 The Depositional History of the Point Pleasant Member of the Cynthiana Formation in Northern Kentucky Gary J. Stefaniak Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Stefaniak, Gary J., "The Depositional History of the Point Pleasant Member of the Cynthiana Formation in Northern Kentucky" (1984). Master's Theses. 1545. https://scholarworks.wmich.edu/masters_theses/1545 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. THE DEPOSITIONAL HISTORY OF THE POINT PLEASANT MEMBER OF THE CYNTHIANA FORMATION IN NORTHERN KENTUCKY by Gary J. Stefaniak A Thesis Submitted to the Faculty o f The Graduate College in partial fulfillm ent of the requirements for the Degree o f Master o f Science Department of Geology Western Michigan U niversity Kalamazoo, Michigan December 1984 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. THE DEPOSITIONAL HISTORY OF THE POINT PLEASANT MEMBER OF THE CYNTHIANA FORMATION IN NORTHERN KENTUCKY Gary J. Stefaniak, M.S. Western Michigan U nive rsity, 1984 Bioclastic limestones, siltstones, and shales of the Point Pleasant Member were deposited in a shallow marine environment immediately below normal e ffe c tiv e wave base. High-energy conditions produced by storms lowered the e ffe ctive wave base and s tirre d the bottom sediments and redistributed them into bedforms.
    [Show full text]
  • Analysis of Appalachia's Utica/Point Pleasant and Marcellus Formations
    Analysis of Appalachia’s Utica/Point Pleasant and Marcellus Formations’ Geology on Estimated Ultimate Recovery Nicholas Cuaresma and Brittany Martin 2019, Marietta College Cuaresma and Martin 2 Abstract: The purpose of this study was to identify the optimum horizontal wellbore azimuths in the Ordovician Utica/Point Pleasant Formation and Devonian Marcellus Formation unconventional petroleum plays in three locations in Ohio, Pennsylvania, and West Virginia, from data contributed by Knobloch Petroleum of Marietta, Ohio. The assumption was that the stress state in the crust determined both the orientations of natural hydraulic fractures formed during the Pennsylvanian Alleghanian orogeny would control the orientation of the fractures formed during present day hydraulic fracturing of horizontal wells. Therefore, the orientation of the horizontal wellbores with respect to fracture orientations would affect the estimated ultimate recovery of petroleum. Multivariable regression analyses, with estimated ultimate recovery as the dependent variable and amount of water used during hydraulic fracturing, amount of sand used as a fracture proppant, and the horizontal wellbore azimuth as the independent variables, were run using data from 1400 wells. A brief overview of the geology of the Appalachian basin, the basin in which both the Utica/Point Pleasant and Marcellus formations were deposited, along with an explanation of the conditions under which natural hydraulic fracturing occurs were included in the study. The study concluded that the amount of water used during hydraulic fracturing in Ohio has the largest effect on the estimated ultimate recovery and the amount of sand used as a fracture proppant in Pennsylvania and West Virginia a numerically large effect on the estimated ultimate recovery, whereas the orientation (azimuth) of the wellbore appears to have an insignificant effect.
    [Show full text]
  • Geochemical Characterization of the Utica Shale Play Using XRF-Based Chemostratigraphy in Ohio
    Stephen F. Austin State University SFA ScholarWorks Electronic Theses and Dissertations Spring 5-4-2021 Geochemical Characterization of the Utica Shale Play using XRF- Based Chemostratigraphy in Ohio Barbara Kemeh [email protected] Julie M. Bloxson Stephen F Austin State University, [email protected] Follow this and additional works at: https://scholarworks.sfasu.edu/etds Part of the Geology Commons Tell us how this article helped you. Repository Citation Kemeh, Barbara and Bloxson, Julie M., "Geochemical Characterization of the Utica Shale Play using XRF- Based Chemostratigraphy in Ohio" (2021). Electronic Theses and Dissertations. 383. https://scholarworks.sfasu.edu/etds/383 This Thesis is brought to you for free and open access by SFA ScholarWorks. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of SFA ScholarWorks. For more information, please contact [email protected]. Geochemical Characterization of the Utica Shale Play using XRF-Based Chemostratigraphy in Ohio Creative Commons License This work is licensed under a Creative Commons Attribution-Noncommercial-No Derivative Works 4.0 License. This thesis is available at SFA ScholarWorks: https://scholarworks.sfasu.edu/etds/383 GEOCHEMICAL CHARACTERIZATION OF THE UTICA SHALE PLAY USING XRF-BASED CHEMOSTRATIGRAPHY IN OHIO By BARBARA M. KEMEH, Bachelor of Science Presented to the Faculty of the Graduate School of Stephen F. Austin State University In Partial Fulfillment Of the Requirements For the Degree of Master of Science STEPHEN F. AUSTIN STATE UNIVERSITY May, 2021 GEOCHEMICAL CHARACTERIZATION OF THE UTICA SHALE PLAY USING XRF-BASED CHEMOSTRATIGRAPHY IN OHIO By BARBARA M. KEMEH, Bachelor of Science APPROVED: Dr.
    [Show full text]
  • Eastern Section American Association of Petroleum Geologists 46Th Annual Meeting Morgantown, West Virginia September 24-27, 2017
    Eastern Section American Association of Petroleum Geologists 46th Annual Meeting Morgantown, West Virginia September 24-27, 2017 Program with Abstracts Hosted by: Appalachian Geological Society West Virginia University Department of Geology and Geography With support from the West Virginia Geological and Economic Survey Meeting Sponsors We appreciate your support! Marcellus Level Meeting Sponsors Utica Level Rogersville Level We appreciate your support! Eastern Section American Association of Petroleum Geologists 46th Annual Meeting Morgantown, West Virginia September 24-27, 2017 Program with Abstracts Hosted by: Appalachian Geological Society West Virginia University Department of Geology and Geography With support from the West Virginia Geological and Economic Survey Cover photo used with permission from Jacob Everhart, Canary, LLC Contents Welcome………………………………………………………………………………………………………………………………………1 2017 Meeting Organizing Committee……………………………………………………………………………….1 Eastern Section AAPG Officers………………………………………………………………………………………….2 Appalachian Geological Society Officers……………………………………………………………………………2 General Information…………………………………………………………………………………………………………………….3 Registration Hours……………………………………………………………………………………………………………3 Parking………………………………………………………………………………………………………………………….….3 Maps………………………………………………………………………………………………………………………………..3 Exhibits……………………………………………………………………………………………………………………….……3 Presenters and Judges Room……………………………………………………………………………………..….…3 Presenters, Judges and Session Chairs Breakfast and Information……………………………………3
    [Show full text]
  • Generalized Correlation Chart of Bedrock Units In
    STATE OF OHIO THIS PUBLICATION WAS FINANCED IN PART THROUGH A GRANT George V. Voinovich, Governor GENERALIZED CORRELATION CHART OF BEDROCK UNITS IN OHIO FROM THE OHIO ENVIRONMENTAL PROTECTION AGENCY DEPARTMENT OF NATURAL RESOURCES UNDER PROVISIONS OF SECTION 319 (h) OF THE CLEAN WATER ACT AS AMENDED IN 1987. Donald C. Anderson, Director OPEN-FILE REPORT 98-2 DIVISION OF GEOLOGICAL SURVEY Compiled by Glenn E. Larsen, September 1998 Thomas M. Berg, Chief EXPLANATION This correlation chart is a product of the Ohio Department of Natural Resources, Division of Root, S. I., Rodriguez, Joaquin, and Forsyth, J. L., 1961, Geology of Knox County: Ohio Division of Kleffner, M. A., 1990, Wenlockian (Silurian) conodont biostratigraphy, depositional environments, and CHRONOSTRATIGRAPHIC UNITS Geological Survey and was prepared as part of a grant (project no. 95 (h) EPA-15) from the Ohio Geological Survey Bulletin 59, 232 p. depositional history along the eastern flank of the Cincinnati Arch in southern Ohio: Journal of Environmental Protection Agency under provisions of Section 319 (h) of the Clean Water Act as Scatterday, J. W., 1963, Stratigraphy and conodont faunas of the Maxville Group (Middle and Upper Paleontology, v. 64, no. 2, p. 319-328. amended in 1987. Funding for the geologic mapping that is the basis for the mapped units shown Mississippian) of Ohio: Ohio State University Ph.D. dissertation (unpub.), The Ohio State Kleffner, M. A., 1994, Conodont biostratigraphy and depositional history of strata comprising the on the chart was provided by the U.S. Geological Survey (National Cooperative Geologic Mapping University, 162 p. Niagaran sequence (Silurian) in the northern part of the Cincinnati Arch region, west-central Ohio, and M NORTH M GLOBAL E AMERICAN AREA 1 AREA 2 AREA 3 AREA 4 AREA 5 AREA 6 AREA 7 AREA 8 AREA 9 AREA 10 AREA 11 AREA 12 AREA 13 AREA 14 Program, STATEMAP component), the Ohio Department of Transportation, and the Ohio Shaver, R.
    [Show full text]
  • SSD Abstract Book Cover 2013.Indd
    Student Scholars Day 4 • 10 • 2013 Elizabeth Uitvlugt Inspiration, Table of Contents 2013 SSD Committee 2 Welcome from Co-Directors 3 Schedule of Events 4 Statement from the Cover Artist 4 Keynote Lecture 5 Henry Hall Map 6 Kirkhof Center Maps 7 & 8 History of SSD 9 History of Undergraduate Research 10 and Scholarship at GVSU McNair Scholars, Student Summer Scholars, 11 and Academic Conference Fund Fredrick Meijer Office of Fellowships 19 fishladder 20 Poster Presentations Schedule and Abstracts 21 Oral Presentations Schedule and Abstracts 84 Panel Presentations Schedule and Abstracts 116 Performance Presentations Schedule and Abstracts 118 Index of Presenters and Mentors 120 Notes 138 SSD Committee Feryal Alayont Mathematics Rebecca Brittian Student Representative Callista Cook Undergraduate Research and Scholarship Alice Chapman History Amanda Cuevas Frederik Meijer Office of Fellowships Robert Deaner Psychology Andrew Lantz Chemistry Susan Mendoza Undergraduate Research and Scholarship (Director) Azizur Molla Anthropology Melissa Morison Classics (Chair) Debbie Morrow Library Ross Reynolds Physics Michael Scantlebury Hospitality and Tourism Management Shelley Sickrey Undergraduate Research and Scholarship Suganthi Sridhar Biomedical Sciences Richard Vallery Physics Patricia Videtich Geology Janet Vigna Biology 2 Welcome to Student Scholars Day 2013! It is with great pleasure that we welcome you to celebrate the diversity and excellence of faculty- student collaboration at GVSU. In its 18th year, Student Scholars Day continues to grow in scope, including six hundred students and mentors in over four hundred presentations. We are excited to support the achievements of these students representing seventy diverse majors across the university. We encourage you to visit presentations of interest in a variety of disciplines and presentation formats, and to engage these students in meaningful discussions of their work.
    [Show full text]
  • EMD Shale Gas and Liquids Committee
    EMD Shale Gas and Liquids Committee 2016 EMD Shale Gas and Liquids Committee Annual Report Ursula Hammes, Chair Bureau of Economic Geology The University of Texas at Austin May 20, 2016 Vice-Chairs: Vice-Chair: Harris Cander (Industry), BP, Houston, TX Vice-Chair: Sven Egenhoff (University), Colorado State University Vice-Chair: Brian Cardott (Government), Oklahoma Geological Survey, Norman, OK Advisory Group: Kent Bowker, Bowker Petroleum, The Woodlands, TX Brian Cardott, Oklahoma Geological Survey, Norman, OK Peng Li, Arkansas Geological Survey, Little Rock, AK Ken Chew, IHS (retired), Perthsire, Scotland Thomas Chidsey, Utah Geological Survey, Salt Lake City, UT Russell Dubiel, U.S. Geological Survey, Denver, CO Catherine Enomoto, U.S. Geological Survey, Reston, VA William Harrison, Western Michigan University, Kalamazoo, MI Ursula Hammes, Bureau of Economic Geology, Austin, TX Shu Jiang, University of Utah, Salt Lake City, UT Julie LeFever, North Dakota Geological Survey, Grand Forks, ND Jock McCracken, Egret Consulting, Calgary, AB Stephan Nordeng, North Dakota Geological Survey, Grand Forks, ND Rich Nyahay, New York Museum, Albany, NY Stephen Sonnenberg, Colorado School of Mines, Golden, CO Beau Tinnin, Pioneer Natural Resources, TX 1 2016 EMD Shale Gas and Liquids Committee Annual Report EXECUTIVE SUMMARY Shale gas and liquids have been the focus of extensive drilling for the past 10+ years due to improved recovery and high oil and gas prices all over the world. Although there is international interest in exploiting hydrocarbons from these unconventional reservoirs, with active exploration projects on most continents, much of the successful exploitation from shales continues to be in North America, particularly in the United States but increasingly so in Canada.
    [Show full text]