Play Analysis of Major Oil Reservoirs in the New Mexico Part of the Permian Basin: Enhanced Production Through Advanced Technologies by Ronald F
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1 Running Head: SEQUENCE STRATIGRAPHY of TEXAS
Running Head: SEQUENCE STRATIGRAPHY OF TEXAS MIDDLE PERMIAN PLATFORM CARBONATES OUTCROP-BASED CHARACTERiZATION OF LEONARDIAN PLATFORM CARBONATE IN WEST TEXAS: IMPLICATIONS FOR SEQUENCE STRATIGRAPHIC STYLES IN TRANSITIONAL ICEHOUSE-GREENHOUSE SETTINGS Stephen C. Ruppel, W. Bruce Ward1, and Eduardo E. Ariza Bureau of Economic Geology The University of Texas at Austin 1 Current address: Earthworks LLC, P.O. Box 178, Newtown, CT 06470-0178 1 ABSTRACT The Sierra Diablo Mountains of West Texas contain world class exposures of lower and middle Permian platform carbonates. As such these outcrops offer key insights into the products of carbonate deposition in the transitional icehouse/greenhouse setting of the early-mid Permian that are available in few other places in the world. They also afford an excellent basis for examing how styles of facies and sequence development vary between platform tops and platform margins. Using outcrop data and observations from over 2 mi (3 km) of continuous exposure, we collected detailed data on the facies composition and architecture of high frequency (cycle-scale) and intermediate frequency (high frequency sequence scale) successions within the Leonardian. We used these data to define facies stacking patterns along depositional dip across the platform in both low and high accommodation settings and to document how these patterns vary systematically between and within sequences . These data not only provide a basis for interpreting similar Leonardian platform successions from less well constrained outcrop and subsurface data sets but also point out some important caveats that should be considered serve as an important model for understanding depositional processes during the is part of the Permian worldwide. -
Geology and Ground-Water Resources of San Miguel County, New Mexico
GEOLOGY AND GROUND - WATER RESOURCES OF SAN MIGUEL COUNTY, NEW MEXICO GROUND-WATER REPORT 2 Geology and Ground-Water Resources of San Miguel County, New Mexico BY R. L. GRIGGS AND G. E. HENDRICKSON Prepared in cooperation with The United States Bureau of Reclamation New Mexico Bureau of Mines & Mineral Resources and the New Mexico State Engineer NEW MEXICO BUREAU OF MINES AND MINERAL RESOURCES SOCORRO 1951 NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Eugene Callaghan, Director THE REGENTS MEMBERS EX-OFFICIO The Honorable Edwin L. Mechem ...................... Governor of New Mexico Tom Wiley ............................................... Superintendent of Public Instruction APPOINTED MEMBERS Thomas M. Cramer, President ...................................................... Carlsbad Holm 0. Bursum, Jr., Secretary-Treasurer ........................................ Socorro Frank C. DiLuzio ..................................................................... Los Alamos A. A. Kemnitz .................................................................................... Hobbs Cooper Shapley ............................................................................... Deming Contents Page ABSTRACT .............................................................................................................. 9 INTRODUCTION ............................................................................................... 11 Location, area, and accessibility 11 Previous investigations -
Permian Basin, West Texas and Southeastern New Mexico
Report of Investigations No. 201 Stratigraphic Analysis of the Upper Devonian Woodford Formation, Permian Basin, West Texas and Southeastern New Mexico John B. Comer* *Current address Indiana Geological Survey Bloomington, Indiana 47405 1991 Bureau of Economic Geology • W. L. Fisher, Director The University of Texas at Austin • Austin, Texas 78713-7508 Contents Abstract ..............................................................................................................................1 Introduction ..................................................................................................................... 1 Methods .............................................................................................................................3 Stratigraphy .....................................................................................................................5 Nomenclature ...................................................................................................................5 Age and Correlation ........................................................................................................6 Previous Work .................................................................................................................6 Western Outcrop Belt ......................................................................................................6 Central Texas ...................................................................................................................7 Northeastern Oklahoma -
Mosaic of New Mexico's Scenery, Rocks, and History
Mosaic of New Mexico's Scenery, Rocks, and History SCENIC TRIPS TO THE GEOLOGIC PAST NO. 8 Scenic Trips to the Geologic Past Series: No. 1—SANTA FE, NEW MEXICO No. 2—TAOS—RED RIVER—EAGLE NEST, NEW MEXICO, CIRCLE DRIVE No. 3—ROSWELL—CAPITAN—RUIDOSO AND BOTTOMLESS LAKES STATE PARK, NEW MEXICO No. 4—SOUTHERN ZUNI MOUNTAINS, NEW MEXICO No. 5—SILVER CITY—SANTA RITA—HURLEY, NEW MEXICO No. 6—TRAIL GUIDE TO THE UPPER PECOS, NEW MEXICO No. 7—HIGH PLAINS NORTHEASTERN NEW MEXICO, RATON- CAPULIN MOUNTAIN—CLAYTON No. 8—MOSlAC OF NEW MEXICO'S SCENERY, ROCKS, AND HISTORY No. 9—ALBUQUERQUE—ITS MOUNTAINS, VALLEYS, WATER, AND VOLCANOES No. 10—SOUTHWESTERN NEW MEXICO No. 11—CUMBRE,S AND TOLTEC SCENIC RAILROAD C O V E R : REDONDO PEAK, FROM JEMEZ CANYON (Forest Service, U.S.D.A., by John Whiteside) Mosaic of New Mexico's Scenery, Rocks, and History (Forest Service, U.S.D.A., by Robert W . Talbott) WHITEWATER CANYON NEAR GLENWOOD SCENIC TRIPS TO THE GEOLOGIC PAST NO. 8 Mosaic of New Mexico's Scenery, Rocks, a n d History edited by PAIGE W. CHRISTIANSEN and FRANK E. KOTTLOWSKI NEW MEXICO BUREAU OF MINES AND MINERAL RESOURCES 1972 NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY STIRLING A. COLGATE, President NEW MEXICO BUREAU OF MINES & MINERAL RESOURCES FRANK E. KOTTLOWSKI, Director BOARD OF REGENTS Ex Officio Bruce King, Governor of New Mexico Leonard DeLayo, Superintendent of Public Instruction Appointed William G. Abbott, President, 1961-1979, Hobbs George A. Cowan, 1972-1975, Los Alamos Dave Rice, 1972-1977, Carlsbad Steve Torres, 1967-1979, Socorro James R. -
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. -
Hypogenic Speleogenesis Within Seven Rivers Evaporites: Coffee Ac Ve, Eddy County, New Mexico Kevin W
Stephen F. Austin State University SFA ScholarWorks Faculty Publications Department of Geology 4-2008 Hypogenic Speleogenesis within Seven Rivers Evaporites: Coffee aC ve, Eddy County, New Mexico Kevin W. Stafford College of Sciences and Mathematics, Department of Geology, Stephen F. Austin State University, [email protected] Lewis Land Alexander Klimchouk Follow this and additional works at: http://scholarworks.sfasu.edu/geology Part of the Geology Commons Tell us how this article helped you. Recommended Citation Stafford, Kevin W.; Land, Lewis; and Klimchouk, Alexander, "Hypogenic Speleogenesis within Seven Rivers Evaporites: Coffee Cave, Eddy County, New Mexico" (2008). Faculty Publications. Paper 10. http://scholarworks.sfasu.edu/geology/10 This Article is brought to you for free and open access by the Department of Geology at SFA ScholarWorks. It has been accepted for inclusion in Faculty Publications by an authorized administrator of SFA ScholarWorks. For more information, please contact [email protected]. K. W. Stafford, L. Land, and A. Klimchouk – Hypogenic speleogenesis within Seven Rivers Evaporites: Coffee Cave, Eddy County, New Mexico. Journal of Cave and Karst Studies, v. 70, no. 1, p. 47–61. HYPOGENIC SPELEOGENESIS WITHIN SEVEN RIVERS EVAPORITES: COFFEE CAVE, EDDY COUNTY, NEW MEXICO KEVIN W. STAFFORD1,2,LEWIS LAND2,3, AND ALEXANDER KLIMCHOUK3,4 Abstract: Coffee Cave, located in the lower Pecos region of southeastern New Mexico, illustrates processes of hypogenic speleogenesis in the middle Permian Seven Rivers Formation. Coffee Cave is a rectilinear gypsum maze cave with at least four stratigraphically-distinct horizons of development. Morphological features throughout the cave provide unequivocal evidence of hypogenic ascending speleogenesis in a confined aquifer system driven by mixed (forced and free) convection. -
Salado Formation Followed
GW -^SZ-i^ GENERAL CORRESPONDENCE YEAR(S): B. QUICK, Inc. 3340 Quail View Drive • Nashville, TN 37214 Phone: (615) 874-1077 • Fax: (615) 386-0110 Email: [email protected] November 12,2002 Mr Roger Anderson Environmental Bureau Chief New Mexico OCD 1220 S. ST. Francis Dr. 1 Santa Fe, NM 87507 Re: Class I Disposal Wells Dear Roger, I am still very interested in getting the disposal wells into salt caverns in Monument approved by OCD. It is my sincere belief that a Class I Disposal Well would be benefical to present and future industry in New Mexico. I suspect that one of my problems has been my distance from the property. I am hoping to find a local company or individuals who can be more on top of this project. In the past conditions have not justified the capital investment to permit, build and operate these wells and compete with surface disposal. Have there been any changes in OCD policy that might effect the permitting of these wells? If so, would you please send me any pretinent documents? Sincerely, Cc: Lori Wrotenbery i aoie or moments rage i uu Ctoraeferiz&MoiHi ©ff Bedded Satt fltoir Storage Caverns Case Stundy from the Midlamdl Basim Susan D. Hovorka Bureau of Economic Geology The University of Texas at Austin AUG1 0R9 9 Environmental Bureau Introduction to the Problem °" Conservation D/ws/on About solution-mined caverns l^Btg*** Geolojy_ofsalt Purpose, scope, and methods of our study Previous work: geologic setting of the bedded salt in the Permian Basin J^rV^W^' " Stratigraphic Units and Type Logs s Midland Basin stratigraphy -
Burned the Crucifixes and Other Religious Objects That Had Been Scattered in and Around the Pueblo. Otermin's Army Repeated This
burned the crucifixes and other religious objects not successful in reestablishing Spanish rule of that had been scattered in and around the the Pueblos, the interviews and explorations pueblo. Otermin's army repeated this ritual at Otermin and Mendoza conducted give the most Alamillo and Sevilleta. A short distance from complete picture of the effects of the revolt Sevilleta the army found deep pits where the among the pueblos. The Spanish presidio at El Indians had cached corn and protected it with a Paso sent two more punitive expeditions to New shrine of herbs. feathers and a clay vessel Mexico in 1688 and 1689 but it was not until the modeled with a human face and the body of a toad term of Governor Don Diego de Vargas (1690-1696) (Hackett and Shelby 1942:I:cxxix). On the march that New Mexico was reclaimed by Spain. from Socorro to Isleta. the army passed through the burned remains of four estancias. The The Aftermath of the Revolt estancia of Las Barrancas, located 23 leagues beyond Senecu and ten leagues downstream from Documentation of the 12-year period following the Isleta, was the only estancia that had not been Pueblo Revolt is scarce but speculation and greatly vandalized and burned (Hackett and Shelby conjecture abound. The more dramatic recon 1942:cxxx). structions of life among the Pueblos after the revolt show the Pueblos having destroyed every Otermin staged a surprise attack, taking Isleta vestige of Hispanic culture, including household Pueblo on December 6, 1681. About 500 Isleta and and religious objects, domesticated animals and Piro Indians were living in the village at the cereal crops. -
Contents • Abbreviations • International Education Codes • Us Education Codes • Canadian Education Codes July 1, 2021
CONTENTS • ABBREVIATIONS • INTERNATIONAL EDUCATION CODES • US EDUCATION CODES • CANADIAN EDUCATION CODES JULY 1, 2021 ABBREVIATIONS FOR ABBREVIATIONS FOR ABBREVIATIONS FOR STATES, TERRITORIES STATES, TERRITORIES STATES, TERRITORIES AND CANADIAN AND CANADIAN AND CANADIAN PROVINCES PROVINCES PROVINCES AL ALABAMA OH OHIO AK ALASKA OK OKLAHOMA CANADA AS AMERICAN SAMOA OR OREGON AB ALBERTA AZ ARIZONA PA PENNSYLVANIA BC BRITISH COLUMBIA AR ARKANSAS PR PUERTO RICO MB MANITOBA CA CALIFORNIA RI RHODE ISLAND NB NEW BRUNSWICK CO COLORADO SC SOUTH CAROLINA NF NEWFOUNDLAND CT CONNECTICUT SD SOUTH DAKOTA NT NORTHWEST TERRITORIES DE DELAWARE TN TENNESSEE NS NOVA SCOTIA DC DISTRICT OF COLUMBIA TX TEXAS NU NUNAVUT FL FLORIDA UT UTAH ON ONTARIO GA GEORGIA VT VERMONT PE PRINCE EDWARD ISLAND GU GUAM VI US Virgin Islands QC QUEBEC HI HAWAII VA VIRGINIA SK SASKATCHEWAN ID IDAHO WA WASHINGTON YT YUKON TERRITORY IL ILLINOIS WV WEST VIRGINIA IN INDIANA WI WISCONSIN IA IOWA WY WYOMING KS KANSAS KY KENTUCKY LA LOUISIANA ME MAINE MD MARYLAND MA MASSACHUSETTS MI MICHIGAN MN MINNESOTA MS MISSISSIPPI MO MISSOURI MT MONTANA NE NEBRASKA NV NEVADA NH NEW HAMPSHIRE NJ NEW JERSEY NM NEW MEXICO NY NEW YORK NC NORTH CAROLINA ND NORTH DAKOTA MP NORTHERN MARIANA ISLANDS JULY 1, 2021 INTERNATIONAL EDUCATION CODES International Education RN/PN International Education RN/PN AFGHANISTAN AF99F00000 CHILE CL99F00000 ALAND ISLANDS AX99F00000 CHINA CN99F00000 ALBANIA AL99F00000 CHRISTMAS ISLAND CX99F00000 ALGERIA DZ99F00000 COCOS (KEELING) ISLANDS CC99F00000 ANDORRA AD99F00000 COLOMBIA -
City of Portales Review of Water Supply Options
CITY OF PORTALES REVIEW OF WATER SUPPLY OPTIONS Prepared for City of Portales Prepared by Charles R. Wilson, Consultant, LLC Santa Fe, New Mexico November 2013 Executive Summary This report presents an overview of optional sources of municipal water supply to supplement Portales’ current supply from the Blackwater Wellfield. Consideration has been given to obtaining supplemental supplies from shallow groundwater, deep groundwater, and surface water from Ute Reservoir. In addition, the report reviews alternatives for reducing water demands including wastewater recycling as well as other water conservation measures. Shallow Groundwater. Shallow groundwater from the Ogallala Aquifer in the vicinity of Portales does not provide a sustainable supply for municipal use. It has become limited in quantity and the City’s Blackwater Wellfield may be unable to support the current rate of use within 10 to 15 years. In the longer term, shallow groundwater can only be considered as a low yield, emergency water source. However, the aquifer could be used to store excess water when available from other sources, such as Ute Reservoir. Deep Groundwater. Deep groundwater from below the Ogallala Aquifer is not a promising water supply alternative for east-central New Mexico. Any water that could be available from this source would be expensive to access, of low quality, and likely also of low quantity. Further, deep groundwater would not be a renewable source of supply. nPursuit of deep groundwater in the Roosevelt – Curry County area would be costly, have a high probability of failure, and is not recommended at this time. Ute Reservoir. A surface water supply from Ute Reservoir on the Canadian River is the only available alternative that would provide Portales with a demonstrated, renewable water supply in sufficient quantity for municipal use. -
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). -
Geologic Map of the Kitchen Cove 7.5-Minute Quadrangle, Eddy County, New Mexico by Colin T
Geologic Map of the Kitchen Cove 7.5-Minute Quadrangle, Eddy County, New Mexico By Colin T. Cikoski1 1New Mexico Bureau of Geology and Mineral Resources, 801 Leroy Place, Socorro, NM 87801 June 2019 New Mexico Bureau of Geology and Mineral Resources Open-file Digital Geologic Map OF-GM 276 Scale 1:24,000 This work was supported by the U.S. Geological Survey, National Cooperative Geologic Mapping Program (STATEMAP) under USGS Cooperative Agreement G18AC00201 and the New Mexico Bureau of Geology and Mineral Resources. New Mexico Bureau of Geology and Mineral Resources 801 Leroy Place, Socorro, New Mexico, 87801-4796 The views and conclusions contained in this document are those of the author and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government or the State of New Mexico. Executive Summary The Kitchen Cove quadrangle lies along the northwestern margin of the Guadalupian Delaware basin southwest of Carlsbad, New Mexico. The oldest rocks exposed are Guadalupian (upper Permian) carbonate rocks of the Seven Rivers Formation of the Artesia Group, which is sequentially overlain by similar strata of the Yates and Tansill Formations of the same Group. Each of these consists dominantly of dolomitic beds with lesser fine-grained siliciclastic intervals, which accumulated in a marine or marginal-marine backreef or shelf environment. These strata grade laterally basinward (here, eastward) either at the surface or in the subsurface into the Capitan Limestone, a massive fossiliferous “reef complex” that lay along the Guadalupian Delaware basin margin and is locally exposed on the quadrangle at the mouths of Dark Canyon and Kitchen Cove.