DOCSLIB.ORG

San Andres Formation Descriptive Geology

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
San Andres Formation Descriptive Geology INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films tfie text directly from the original or copy submitted. Thus, some tfiesis and dissertation copies are in typewriter face, wttile 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 tfie autfior did not send UMI a complete manuscript and there are missing pages, tfiese wiH be noted. Also, if unautfiorized copyright material fiad 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 comer and continuing from left to right in equal sections with small overlaps. Photographs included in tfie original manuscript fiave been reproduced xerographically in this copy. Higfier quality 6" x 9" tilack and vriiite pfiotographic prints are available for any photographs or illustrations appearing in this copy for an additional cfiarge. Contact UMI directly to order. Bell & Howell Information and teaming 300 North Zeeb Road, Ann Arbor, Ml 48106-1346 USA 800-521-0600 UMI* NOTE TO USERS This reproduction is the best copy available. UMI UNIVERSITY OF OKLAHOMA GRADUATE COLLEGE RESERVOIR CHARACTERIZATION AND GEOSTATISTICAL MODELING OF THE WEST JORDAN UNIT SAN ANDRES FORMATION, CENTRAL BASIN PLATFORM, ECTOR AND CRANE COUNTIES, WEST TEXAS A DISSERTATION SUBMITTED TO THE GRADUATE FACULTY in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY By VICTORIA POLZIN-FRENCH Norman, Oklahoma 2000 UMI Number 9964629 UMI* UMI Microform9964629 Copyright 2000 by Bell & Howell Information and teaming Company. All rights reserved. This microform edition is protected against unauthorized copying under Title 17, United States Code. Bell & Howell Information and teaming Company 300 North Zeeb Road P.O. Box 1346 Ann Arbor. Ml 48106-1346 RESERVOIR CHARACTERIZATION AND GEOSTATISTICAL MODELING OF THE WEST JORDAN UNIT SAN ANDRES FORMATION, CENTRAL BASIN PLATFORM, ECTOR AND CRANE COUNTIES, WEST TEXAS A Dissertation APPROVED FOR THE DEPARTMENT OF GEOLOGY AND GEOPHYSICS BY Copyright by VICTORIA POLZIN-FRENCH 2000 Ail Rights Reserved ACKNOWLEDGMENTS Texaco Exploration and Production, Inc (TEPI) have graciously provided funding for this study not only through generous financial support but also by providing all necessary data needed to complete the study. In addition many individuals have provided professional and technical guidance which has made the completion of this study possible. 1 would like to thank the following professors at the University of Oklahoma for their continuous support while serving as committee members for this study; Dr. James M. Forgotson, Dr. Daniel J. O’Meara, Dr. Thomas A. Dewars, and Dr. Mark Morrissey. In addition, I would like to thank Dr. W. G. Brown (Baylor University), for serving as the outside member of the dissertation committee and for all the help and inspiration he has given me throughout my years spent at Baylor. I would like to give particular thanks to Anna Shaughnessy, Texaco Group Inc., for her interest in the Institute for Reservoir Characterization at the University of Oklahoma. Anna initiated this study by directing me to Texaco Exploration and Production, Inc (TEPI) scientists who worked together with committee members and myself to develop a suitable project. A number of people at TEPl’s Midland, Texas office have provided guidance and knowledge of the Permian basin area. 1 would like to thank Kim Moore, Monty Fields and Julie Gibbs for proposing the project. Kim has been my mentor through the project and given me much insight to the Permian basin area and provided considerable support in all aspects of the project where needed. Monty has helped me to understand the engineering aspects of the West Jordan unit and fluid movement through the reservoir. 1 would also like to thank Robert McKnaughton for long discussions on waterflood iv management, particularly with respect to fluid movement and water chemistry within a waterflood environment and the considerable changes that can occur within a water- flooded reservoir. I would also like to thank Curtis Horn for showing me seismic data surrounding the West Jordan unit which enabled me to have a better understanding o f broad seismic stratigraphie relationships of the San Andres Formation from the Midland basin onto the Central Basin platform. Appreciation is also extended to Dan George who aided me with a more regional structural analysis of the area surrounding the West Jordan unit. Very special thanks are extended to Dr. Susan Longacre, Texaco Upstream Technology (TU) Department, Houston, Texas, for many hours spent guiding me through the world of carbonates and how they relate to the Permian Basin. Her expertise and input of core studies were instrumental to the understanding of the complexities of dolomitized rocks, their depositional environments, facies, and cyclic nature. Susan laid the foundation on which all my subsequent learning in the world of carbonates has been built. Mike Crammer, also at TU, was extremely helpful with describing facies partitioning within cycle boundaries and provided many useful suggestions for pulling all the chronostratigraphic work together. His suggested improvements on several figures seen within the text were sincerely appreciated. In addition, Mike provided use to his high powered microscope for analysis of samples under ultra violet florescence. Gratitude is extended to Greg Hinterlong “the man who never sleeps” with the COi Asset Team (TEPI, Midland, Texas). Greg provided insight into a number of topics affecting carbonate reservoirs including: petrophysical properties associated with San Andres dolomites; fluid flow within the reservoir; chronostratigraphic relationships within carbonate ramp settings; and extensive discussions on depositional environments and the diagenetic events that that have influenced production within these rocks. Greg has also provided considerable help in maneuvering through the geostatistical program and explaining key concepts when needed. Greg has always made himself available to answer any questions or address concerns with the project and his efforts are sincerely appreciated. I would also like to thank all the regular members of the Texaco “Carbonate Café” lunch group not already mentioned including: Emily Stoudt, David Sivils, Mike Raines, Cory Hoffinan. Denise Pfefifer, Dennis Dull and Dennis Prezbindowski. This group has provided informative presentations and discussions on carbonate reservoirs that have enhanced my knowledge considerably. Bill Keyser and Dave Liebman of TEPI, Midland Texas, provided assistance with reformatting grid files so that they could be imported into StrataModel and Earth Vision three dimensional visualization programs. Without their help building a complete visualization model would have been a tedious and much longer process. 1 would like to thank Steve Ruppel, Mark Holtz and Rick Major from the Bureau of Economic Geology, University of Texas. Information related to San Andres production within neighboring units was provided by these three gentlemen. Steve and Rick showed me core from the area and discussed their interpretations during a visit to the BEG. Mark provided me with data and information from work that he completed on the Jordan University Unit. 1 would also like to thank James Dormelly for many hours spent on the phone with me coordinating the shipment of BEG cores from Austin to the University of Oklahoma and Midland, Texas. Appreciation is also extended to OXY USA, Inc., for giving me permission to use one of their seismic lines within the body of vi this paper. In addition to the people mentioned above, a vast number of individuals have given me moral support and assistance throughout the completion of this study. 1 would like to thank everyone within the TEPI former Central Basin Platform Asset Team and individuals within the Midland Asset Team and associated operating units who have supplied me with data or support. 1 would particularly like to thank the members of my team who have been supportive and understanding while 1 have taken time to finish this project including: Ryan Ott, Shilpa Abbitt, Bob Johnson, Curtis Horn, Kim Moore, Jim Ferrell, and Steve Chandler. 1 would like to thank Patrick J. O’Connell for his emotional support and “you need to wrap it up girl” comments to help me stay focused; Brenda Braun for getting me out on the town on occasion, and Dinero for all the stress relieving rides. Finally, 1 thank my family for their continued support and encouragement without which this study would never have been possible. My mother Patsy A. Polzin has always encouraged me to be independent and motivated me to pursue my goals, my father Earl A. Polzin has provided me with a great respect for all individuals and high admiration for moral character while encouraging me to follow my heart and dreams, and my brother Douglas L. Polzin who has always been around for me when 1 need emotional support in my life or a ski buddy to get away for a while and play in the snow. Thank you all. VII TABLE OF CONTENTS ACKNOWLEDGMENTS...............................................................................................iv CONTENTS ......................................................................................................................viii
Load more

Recommended publications
  • Speleogenesis and Delineation of Megaporosity and Karst
    Stephen F. Austin State University SFA ScholarWorks Electronic Theses and Dissertations 12-2016 Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas Jon T. Ehrhart Stephen F. Austin State University, [email protected] Follow this and additional works at: https://scholarworks.sfasu.edu/etds Part of the Geology Commons, Hydrology Commons, and the Speleology Commons Tell us how this article helped you. Repository Citation Ehrhart, Jon T., "Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas" (2016). Electronic Theses and Dissertations. 66. https://scholarworks.sfasu.edu/etds/66 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]. Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas 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/66 Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas By Jon Ehrhart, B.S. 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.
    [Show full text]
  • Mineral and Energy Resources of the BLM Roswell Resource Area, East-Central New Mexico
    U. S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY Mineral and Energy Resources of the BLM Roswell Resource Area, East-central New Mexico by Susan Bartsch-Winkleri, editor Open-File Report 92-0261 1992 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1 Denver, Colorado iMail Stop 937 Federal Center P.O. Box 25046 Denver, Colorado 80225 MINERAL AND ENERGY RESOURCES OF THE BLM ROSWELL RESOURCE AREA, EAST-CENTRAL NEW MEXICO Summary.......................................................................................... 1 Introduction.................................................................................... 1 Location and geography of study area...................................... 1 Purpose and methodology........................................................ 3 Acknowledgements......................................................................... 4 Geology of east-central New Mexico, by Susan Bartsch-Winkler, with a section on Intrusive and extrusive alkaline rocks of the Lincoln County porphyry belt by Theodore J. Armbrustmacher 4 General..................................................................................... 4 Structure................................................................................. 5 Uplifts........................................................................
    [Show full text]
  • San Andres Formation
    StephenStephen C.C. Ruppel,Ruppel, SUBREGIONALSUBREGIONAL DEVELOPMENTDEVELOPMENT OFOF RESERVOIRRESERVOIR POROSITYPOROSITY ATAT AA MAJORMAJOR PERMIANPERMIAN UNCONFORMITY:UNCONFORMITY: BureauBureau ofof EconomicEconomic Geology,Geology, SANSAN ANDRESANDRES FORMATION,FORMATION, WESTWEST TEXASTEXAS TheThe UniversityUniversity ofof Texas,Texas, Austin,Austin, TX,TX, 78713-892478713-8924 ABSTRACTABSTRACT Most porosity development in carbonate reservoirs can be attributed in part or in total to diagenesis. This is especially true in Permian reservoirs of the Permian Basin, nearly all of which are dolomitized. Linking this diagenesis and associated porosity to unconformities representing major falls in sea level, INTRODUCTIONINTRODUCTION STRATIGRAPHYSTRATIGRAPHY ANDAND FACIESFACIES however, is commonly problematic using typical reservoir data sets. New subsurface data from the San Andres Formation, a major oil-producing reservoir in Texas and New Mexico, coupled with relationships previously defined from SANSAN ANDRES-GRAYBURGANDRES-GRAYBURG STRATIGRAPHYSTRATIGRAPHY ANDAND FACIESFACIES CYCLECYCLE STRATIGRAPHYSTRATIGRAPHY ANDAND FACIESFACIES ARCHITECTUREARCHITECTURE equivalent outcrops, illustrate both the style and expression of such porosity SANSAN ANDRESANDRES STRUCTURESTRUCTURE FUHRMAN-MASCHOFUHRMAN-MASCHO FIELDFIELD Fuhrman-MaschoFuhrman-Mascho FieldField Fuhrman-MaschoFuhrman-Mascho SanSan AndresAndres Field,Field, AndrewsAndrews County,County, TexasTexas development. MIDDLE PERMIAN SEQUENCE STRATIGRAPHY ty Northwest Southeast MIDDLE PERMIAN SEQUENCE STRATIGRAPHY i -1100 PSL A-43 PermianPermian BasinBasin Gamma ray (API) Neutron porosity (%) PSL A-47 Depth Although the San Andres is characterized by an upward-shallowing succession Oil FMU 12A FMU 211 FMU 607 FMU 605 FMU 705 FMU 806 (ft) WFMU 110 WFMU 109 aturation WFMU 124 GR N GR N GR N GR N High Western Central Western 0 100 30 20 1010 0 -10 s GR N GR N of outer- to inner-ramp carbonate lithofacies in most platform settings, pervious Relative Algerita Western Permeabil GR N GR N ft GDP ft ft ft ft freq.
    [Show full text]
  • Play Analysis and Digital Portfolio of Major Oil Reservoirs in the Permian Basin
    Play Analysis and Digital Portfolio of Major Oil Reservoirs in the Permian Basin: Application and Transfer of Advanced Geological and Engineering Technologies for Incremental Production Opportunities Final Report Reporting Period Start Date: January 14, 2002 Reporting Period End Date: May 13, 2004 Shirley P. Dutton, Eugene M. Kim, Ronald F. Broadhead, Caroline L. Breton, William D. Raatz, Stephen C. Ruppel, and Charles Kerans May 2004 Work Performed under DE-FC26-02NT15131 Prepared by Bureau of Economic Geology John A. and Katherine G. Jackson School of Geosciences The University of Texas at Austin University Station, P.O. Box X Austin, TX 78713-8924 and New Mexico Bureau of Geology and Mineral Resources New Mexico Institute of Mining and Technology Socorro, NM 87801-4681 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, express or implied, or assumes any legal liability for responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe 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. iii ABSTRACT The Permian Basin of west Texas and southeast New Mexico has produced >30 Bbbl (4.77 × 109 m3) of oil through 2000, most of it from 1,339 reservoirs having individual cumulative production >1 MMbbl (1.59 × 105 m3).
    [Show full text]
  • Outcropping Permian Shelf Formations of Eastern New Mexico Vincent C
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/23 Outcropping Permian shelf formations of eastern New Mexico Vincent C. Kelley, 1972, pp. 72-78 in: East-Central New Mexico, Kelley, V. C.; Trauger, F. D.; [eds.], New Mexico Geological Society 23rd Annual Fall Field Conference Guidebook, 236 p. This is one of many related papers that were included in the 1972 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States.
    [Show full text]
  • Capitan Reef Complex Structure and Stratigraphy
    Capitan Reef Complex Structure and Stratigraphy Report by Allan Standen, P.G. Steve Finch, P.G. Randy Williams, P.G., Beronica Lee-Brand, P.G. Assisted by Paul Kirby Texas Water Development Board Contract Number 0804830794 September 2009 TABLE OF CONTENTS 1. Executive summary....................................................................................................................1 2. Introduction................................................................................................................................2 3. Study area geology.....................................................................................................................4 3.1 Stratigraphy ........................................................................................................................4 3.1.1 Bone Spring Limestone...........................................................................................9 3.1.2 San Andres Formation ............................................................................................9 3.1.3 Delaware Mountain Group .....................................................................................9 3.1.4 Capitan Reef Complex..........................................................................................10 3.1.5 Artesia Group........................................................................................................11 3.1.6 Castile and Salado Formations..............................................................................11 3.1.7 Rustler Formation
    [Show full text]
  • "Geology & Ground-Water Conditions in Southern Lea County, New
    ItI *1. I.4 GROUND-WTATER REPORT 6 an4 A.; Geology and Ground-Water 54 Conditions in Southern I Lea County, New Mexico by ALEXANDER NICHOLSON, Jr. C,'I and ALFRLD CLEBSCH, JR. UN!TED STATES GEOLOGICAL SUR'VEY i I I i i I i I' ;it it. STATE BUREAU OF MINES AND MINERAL RESOURCES .t64 NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO Contents Page NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY ABSTRACT ............................................. 1 E. J. Workman, President INTRODUCTION ....................................... 2 Location and area ....................................... 2 History and scope of investigation ......................... 2 STATE BUREAU OF MINES AND MINERAL RESOURCES Previous investigations and acknowledgments ............... 4 Well-numbering system ................................. 5 Alvin J. Thompson, Direclor GEOGRAPHY ............... 7 Topography and drainage ................................ 7 Mescalero Ridge and High Plains ....................... 7 THE REGENTS Querecho Plains and Laguna Valley ..................... 9 Grama Ridge area ..................................... 11 MEEMBERS Ex OFFICIO Eunice Plain ......................................... 12 Monument Draw ................................... 12 TheHonorable Edwin L. Mechern ...... Governor of New Mexico Rattlesnake Ridge area ................................ 13 Tom Wiley ............. Superintendent of Public Instruction San Simon Swale ...................................... 13 Antelope Ridge area .................................
    [Show full text]
  • The Oil and Gas Resources of New Mexico SECOND EDITION
    NEW MEXICO SCHOOL OF MINES BULLETIN 18 STATE BUREAU OF MINES AND MINERAL RESOURCES PLATE 1 Ship Rock, northwestern San Juan County. An igneous intrusion with radiating dikes. In the Rattle- snake pool, less than five miles away, oil and gas have accumulated in Cretaceous strata similar to those in the foreground. (Spence Air Photos.) NEW MEXICO SCHOOL OF MINES STATE BUREAU OF MINES AND MINERAL RESOURCES RICHARD H. REECE President and Director BULLETIN NO. 18 The Oil and Gas Resources of New Mexico SECOND EDITION Compiled by ROBERT L. BATES Geologist, State Bureau of Mines and Mineral Resources SOCORRO, NEW MEXICO 1942 CONTENTS Page The State Bureau of Mines and Mineral Resources ---------------------------------------------------- 12 Board of Regents ------------------------------------------------------------------------------------- 12 Introduction, by Robert L. Bates -------------------------------------------------------------------------- 13 General statement ------------------------------------------------------------------------------------- 13 Purpose and scope of the report -------------------------------------------------------------------- 13 Acknowledgments -------------------------------------------------------------------------------------14 Geography and general geology, after D. E. Winchester ---------------------------------------------- 15 The Rocks ---------------------------------------------------------------------------------------------------- 18 General statement, by Robert L. Bates ------------------------------------------------------------
    [Show full text]
  • STE K' Portions of This Domlmmt May Be Illegible in Electronic Image Products
    DOE/BC/I 4895-10 Distribution Category UC-122 Effects of Stratal Architecture and Diagenesis on Reservoir Development in the Grayburg Formation: South Cowden Field, Ector County, Texas Annual Report for the Period October 1, 1994 to September 30, 1995 BY Stephen Ruppel Don Bebout February 1996 Work Performed Under Contract No. DE-AC22-93BC14895 Prepared for U.S. Department of Energy Assistant Secretary for Fossil Energy Robert Lemmon, Project Manager Bartlesville Project Off ice P.O. Box 1398 Bartlesville, OK 74005 Prepared by The University of Texas at Austin Bureau of Economic Geology Austin, TX 78713-7508 STE k' Portions of this domlmmt may be illegible in electronic image products. are produced from the best available original dOCUXXl€!XlL CONTENTS ABSTRACT .................................................................................................................................... 1 INTRODUCTION .......................................................................................................................... 2 SETI'ING ........................................................................................................................................ 4 METHODS ..................................................................................................................................... 6 REGIONAL GEOLOGICAL SE'ITING ........................................................................................ 6 GRAYBURG DEPOSITIONAL FACIES IN SOUTH COWDEN FIELD ................................. 18 Fusulinid Wackestone
    [Show full text]
  • Sequence Stratigraphic Framework of the Upper San Andres Formation and Equivalent Basinal Strata in the Brokeoff Mountains, Otero County, New Mexico William M
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/44 Sequence stratigraphic framework of the upper San Andres Formation and equivalent basinal strata in the Brokeoff Mountains, Otero County, New Mexico William M. Fitchen, 1993, pp. 185-193 in: Carlsbad Region (New Mexico and West Texas), Love, D. W.; Hawley, J. W.; Kues, B. S.; Austin, G. S.; Lucas, S. G.; [eds.], New Mexico Geological Society 44th Annual Fall Field Conference Guidebook, 357 p. This is one of many related papers that were included in the 1993 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks.
    [Show full text]
  • DOCTOR of PHILOSOPHY (Ph.D.)
    Establishing a Tephrochronologic Framework for the Middle Permian (Guadalupian) Type Area and Adjacent Portions of the Delaware Basin and Northwestern Shelf, West Texas and Southeastern New Mexico, USA A dissertation submitted to the Graduate School of the University of Cincinnati In partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY (Ph.D.) In the Department of Geology Of the McMicken College of Arts and Sciences 2011 by Brian Lee Nicklen B.S. University of Nebraska-Lincoln, 2001 M.S. University of Cincinnati, 2003 Committee Members: Prof. Warren D. Huff (Ph.D.), Chair Prof. Carlton E. Brett (Ph.D.) Prof. Attila I. Kilinc (Ph.D.) Prof. J. Barry Maynard (Ph.D.) Dr. Gorden L. Bell Jr. Prof. Scott D. Samson (Ph.D.) Abstract DesPite being recognized for many years, bentonites in the Middle Permian (Guadalupian Series) type area of west Texas and southeastern New Mexico, have received little research attention. As these important dePosits act as geologic timelines, they can be used as tools for long distance stratigraphic correlation and high-precision radioisotopic age dating. An important Problem that these bentonites can address is the lack of temporal control for the Guadalupian. This is an important time interval for significant changes in Earth’s climate and biodiversity that include events leading uP to, and Potentially including, the first pulse of a double-Phase mass extinction at the end of the Paleozoic. Also needed is better temporal constraint for key GuadaluPian global chemostratigraPhic and geomagnetic markers. In light of this, the duration of the Guadalupian stages and boundary age estimations need to be updated in order to assess cause and effect of these significant events.
    [Show full text]
  • HI-RES Final Report
    Development of an Advanced Approach for Next-Generation Integrated Reservoir Characterization Final Report Period of Performance: October 1, 2001 – December 31, 2004 Authored By: Scott R. Reeves Advanced Resources International, Inc. Performed By: Advanced Resources International, Inc. 9801 Westheimer, Suite 805 Houston, Texas 77042 U.S. Department of Energy Award Number DE-FC26-01BC15357 April, 2005 Advanced Resources International Disclaimers 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, express 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 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. Advanced Resources International Disclaimer The material in this Report is intended for general information only. Any use of this material in relation to any specific application should be based on independent examination and verification of its unrestricted applicability for such use and on a determination of suitability for the application by professionally qualified personnel. No license under any Advanced Resources International, Inc., patents or other proprietary interest is implied by the publication of this Report.
    [Show full text]