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University of Oklahoma Graduate College
UNIVERSITY OF OKLAHOMA GRADUATE COLLEGE POTENTIAL FIELD STUDIES OF THE CENTRAL SAN LUIS BASIN AND SAN JUAN MOUNTAINS, COLORADO AND NEW MEXICO, AND SOUTHERN AND WESTERN AFGHANISTAN A DISSERTATION SUBMITTED TO THE GRADUATE FACULTY in partial fulfillment of the requirements for the Degree of DOCTOR OF PHILOSOPHY By BENJAMIN JOHN DRENTH Norman, Oklahoma 2009 POTENTIAL FIELD STUDIES OF THE CENTRAL SAN LUIS BASIN AND SAN JUAN MOUNTAINS, COLORADO AND NEW MEXICO, AND SOUTHERN AND WESTERN AFGHANISTAN A DISSERTATION APPROVED FOR THE CONOCOPHILLIPS SCHOOL OF GEOLOGY AND GEOPHYSICS BY _______________________________ Dr. G. Randy Keller, Chair _______________________________ Dr. V.J.S. Grauch _______________________________ Dr. Carol Finn _______________________________ Dr. R. Douglas Elmore _______________________________ Dr. Ze’ev Reches _______________________________ Dr. Carl Sondergeld © Copyright by BENJAMIN JOHN DRENTH 2009 All Rights Reserved. TABLE OF CONTENTS Introduction…………………………………………………………………………..……1 Chapter A: Geophysical Constraints on Rio Grande Rift Structure in the Central San Luis Basin, Colorado and New Mexico………………………………………………………...2 Chapter B: A Geophysical Study of the San Juan Mountains Batholith, southwestern Colorado………………………………………………………………………………….61 Chapter C: Geophysical Expression of Intrusions and Tectonic Blocks of Southern and Western Afghanistan…………………………………………………………………....110 Conclusions……………………………………………………………………………..154 iv LIST OF TABLES Chapter A: Geophysical Constraints on Rio Grande Rift Structure in the Central -
Listado Con Los Perfiles Seleccionados Que Pasan a La Etapa
INSTITUTO ELECTORAL DEL ESTADO SECRETARÍA EJECUTIVA DIRECCIÓN DE ORGANIZACIÓN ELECTORAL LISTADO CON LOS PERFILES SELECCIONADOS QUE PASAN A LA ETAPA DE COTEJO DOCUMENTAL Y APLICACIÓN DEL FORMATO DE ENTREVISTA DEL PROCESO DE SELECCIÓN Y DESIGNACIÓN DE LOS CONSEJOS MUNICIPALES ELECTORALES APELLIDO APELLIDO CARGO AL QUE VALORACION VALORACION Y DTTO MUNICIPIOFOLIO NOMBRE GENERO EXAMEN (%) PATERNO MATERNO ASPIRA CURRICULAR (%) EXAMEN 1 FRANCISCO Z. MENA 65 40 ANALLELY RAMIREZ QUIROZ AMBOS M 23.75 8.5 32.25 1 FRANCISCO Z. MENA 65 25 CLAUDIO VARGAS HERNANDEZ AMBOS H 21.25 8.5 29.75 1 FRANCISCO Z. MENA 65 4 ANGELICA JULIAN MARIA CE M 20 8.5 28.5 1 FRANCISCO Z. MENA 65 38 HECTOR JESUS AVILA LEYVA AMBOS H 21.25 8 29.25 1 FRANCISCO Z. MENA 65 8 ALMABETH BERMUDEZ VELAZQUEZ CE M 17.5 8.5 26 1 FRANCISCO Z. MENA 65 37 ADAN PEREZ HERNANDEZ AMBOS H 20 8.5 28.5 1 FRANCISCO Z. MENA 65 10 ORQUIDEA RODRIGUEZ MONTERO CE M 17.5 8.5 26 1 FRANCISCO Z. MENA 65 5 JUAN LUIS OSORIO TELLEZ CE H 20 8 28 1 FRANCISCO Z. MENA 65 14 CARMELA CRUZ MARTINEZ SE M 17.5 8.5 26 1 FRANCISCO Z. MENA 65 9 RAUL MARTIN GARCIA CE H 17.5 8 25.5 1 FRANCISCO Z. MENA 65 7 YULIANA HERNANDEZ SANTIAGO CE M 16.25 8.5 24.75 1 FRANCISCO Z. MENA 65 3 ALBERTO SOLIS GARCIA CE H 17.5 8 25.5 1 FRANCISCO Z. MENA 65 20 CARMEN SANTIAGO APARICIO AMBOS M 17.5 7 24.5 1 FRANCISCO Z. -
Southern Mexico): Implications for the Evolution of the Iapetus and Rheic Oceans
Pressure-temperature-time evolution of Paleozoic high-pressure rocks of the Acatlán Complex (southern Mexico): Implications for the evolution of the Iapetus and Rheic Oceans Ricardo Vega-Granillo† Departamento de Geología, Universidad de Sonora, Rosales y Encinas S/N, Hermosillo, Sonora, México 83000 Oscar Talavera-Mendoza Unidad Académica de Ciencias de la Tierra, Universidad Autónoma de Guerrero, A.P. 197, Taxco, Guerrero, México 40200 Diana Meza-Figueroa Departamento de Geología, Universidad de Sonora, Rosales y Encinas S/N, Hermosillo, Sonora, México 83000 Joaquin Ruiz George E. Gehrels Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA Margarita López-Martínez Departamento de Geología, CICESE, Km 107 Carr, Tijuana–Ensenada, Ensenada, Baja California, México Julio C. de la Cruz-Vargas Departamento de Geología, Universidad de Sonora, Rosales y Encinas S/N, Hermosillo, Sonora, México 83000 ABSTRACT 830–730 °C and 17–15 kb. Amphibole from INTRODUCTION eclogite yields a 430 ± 5 Ma 40Ar/39Ar age, dat- New thermobarometric and U/Pb and ing the high-pressure (HP) event. P-T paths of Owing to their tectonic setting and viability 40Ar/39Ar geochronologic data coupled with high-temperature (HT) eclogites like those of for providing quantitative thermobarometric and ages obtained from the Acatlán Complex, the the Esperanza suite have been related to the geochronological measurements, high-pressure basement of the Mixteco terrane of southern collision of continental blocks. Partial over- (HP) assemblages are frequently used to recon- Mexico, reveal the existence of three distinc- printing occurred at 690–640 °C and 14–10 kb struct the tectonic evolution of ancient orogenic tive high-pressure metamorphic events of prior to 374 ± 2 Ma (40Ar/39Ar, phengite). -
Polyphase Deformation in San Miguel Las Minas, Northern
POLYPHASE DEFORMATION IN SAN MIGUEL LAS MINAS, NORTHERN ACATLAN COMPLEX, SOUTHERN MEXICO A thesis presented to the faculty of the Arts and Sciences of Ohio University In partial fulfillment of the requirements for the degree Master of Sciences Brent J. Barley August 2006 This thesis entitled POLYPHASE DEFORMATION IN SAN MIGUEL LAS MINAS, NORTHERN ACATLAN COMPLEX, SOUTHERN MEXICO by BRENT J. BARLEY has been approved for the Department of Geological Sciences and the College of Arts and Sciences by R. Damian Nance Professor of Geological Sciences Benjamin M. Ogles Dean, College of Arts and Sciences Abstract BARLEY, BRENT J., M.S., August 2006, Geological Sciences POLYPHASE DEFORMATION IN SAN MIGUEL LAS MINAS, NORTHERN ACATLAN COMPLEX, SOUTHERN MEXICO (58 pages) Director of Thesis: R. Damian Nance Mapping in the northern part of the Acatlán Complex (southern Mexico) has distinguished two lithological units: a high-grade unit assigned to the Piaxtla Suite, and a low-grade unit assigned to the Cosoltepec Formation. Two major Paleozoic tectonothermal events have been identified in these rocks. The first event produced a penetrative deformational fabric (SPS1) parallel to a compositional banding during blueschist and amphibolite facies metamorphism, which has recently been dated as ~346 Ma in a neighboring area, and a greenschist overprint during exhumation. The second event, which is recorded in both the Piaxtla Suite and Cosoltepec Formation, produced two penetrative deformational fabrics under subgreenschist metamorphic conditions. The first, high-grade tectonothermal event accompanied closure of the Rheic Ocean and tectonic juxtapositioning of the two units during exhumation of the high-grade unit in the Devono-Carboniferous. -
LEY DE INGRESOS DEL MUNICIPIO DE NAUZONTLA, Para El Ejercicio Fiscal 2021
GOBIERNO CONSTITUCIONAL DEL ESTADO DE PUEBLA PERIÓDICO OFICIAL LAS LEYES, DECRETOS Y DEMÁS DISPOSICIONES DE CARÁCTER OFICIAL SON OBLIGATORIAS POR EL SOLO HECHO DE SER PUBLICADAS EN ESTE PERIÓDICO Autorizado como correspondencia de segunda clase por la Dirección de Correos con fecha 22 de noviembre de 1930 Nahúm Rene Santaella Vázquez NÚMERO 18 “CUATRO VECES HEROICA PUEBLA DE ZARAGOZA” TOMO DXLVIII CUARTA JUEVES 24 DE DICIEMBRE DE 2020 SECCIÓN Sumario GOBIERNO DEL ESTADO PODER LEGISLATIVO DECRETO del Honorable Congreso del Estado, por el que expide la LEY DE INGRESOS DEL MUNICIPIO DE NAUZONTLA, para el Ejercicio Fiscal 2021. DECRETO del Honorable Congreso del Estado, por el cual e xpide la Zonificación Catastral y las Tablas de Valores Unitarios de Suelos Urbanos y Rústicos; así como los Valores Catastrales de Construcción por metro cuadrado, para el Municipio de Nauzontla. Jueves 24 de diciembre de 2020 Periódico Oficial del Estado de Puebla (Cuarta Sección) 3 GOBIERNO DEL ESTADO PODER LEGISLATIVO DECRETO del Honorable Congreso del Estado, por el que expide la LEY DE INGRESOS DEL MUNICIPIO DE NAUZONTLA, para el Ejercicio Fiscal 2021. Al margen el Escudo del Estado de Puebla, con una leyenda que dice: Unidos en el Tiempo, en el Esfuerzo, en la Justicia y en la Esperanza. Estado Libre y Soberano de Puebla. H. Congreso del Estado de Puebla. LX Legislatura. LUIS MIGUEL GERÓNIMO BARBOSA HUERTA, Gobernador Constitucional del Estado Libre y Soberano de Puebla, a sus habitantes sabed: Que por la Secretaría del H. Congreso, se me ha remitido el -
New Mexico Geological Society Spring Meeting Abstracts
include allowing growth to become dependent in the Taos region; an inventory and geochemi- on a continually shrinking supply, responsibility cal study of the springs in the Rio Grande gorge; Abstracts for the perpetual pumping, and commitment of a paleoseismic trenching study of the southern future energy resources. Sangre de Cristo fault near Taos; and a study of the geology, hydrogeology, and hydrogeochem- INVITED SPEAKERS istry of surface water/ground water interactions along the Rio Grande in northern Taos County. New Mexico Geological Society THE SAN LUIS BASIN OF THE NORTHERN The Taos Soil & Water Conservation District has spring meeting RIO GRANDE RIFT, P. W. Bauer, bauer@nmt. inventoried water wells and mapped the ground edu, New Mexico Bureau of Geology and water and water quality of the county. Over The New Mexico Geological Society annual Mineral Resources, New Mexico Institute of many years, Glorieta Geoscience, Inc., has inves- spring meeting was held on April 18, 2008, at Mining and Technology, Socorro, New Mexico tigated the hydrogeology, aquifer characteristics, Best Western Convention Center, Socorro. Fol- 87801 and hydrogeochemistry of the Taos region. lowing are the abstracts from all sessions given The San Luis Basin (SLB) is the northernmost at that meeting. large basin of the Rio Grande rift. It extends EVOLVING GEOLOGIC UNDERSTANDING about 240 km from Velarde, New Mexico, to OF THE ESPAÑOLA BASIN, RIO GRANDE Keynote presentation p. 52 Poncha Pass, Colorado, encompassing the San RIFT, NORTHERN NEW MEXICO, G. A. Invited speakers p. 52 Luis Valley to the north and the Taos Plateau to Smith, [email protected], Department of Earth Session 1—Rio Grande rift, San Luis and Española the south. -
(Southern Mexico): Implications for the Evolution of the Iapetus and Rheic Oceans: Reply
Pressure-temperature-time evolution of high-pressure rocks of the Acatlán Complex (southern Mexico): Implications for the evolution of the Iapetus and Rheic Oceans: Reply Ricardo Vega-Granillo1,†, Oscar Talavera-Mendoza2, Diana Meza-Figueroa1, Joaquin Ruiz3, Margarita López-Martínez4, and George E. Gehrels3 1Departamento de Geología, Universidad de Sonora, Rosales y Encinas S/N, Hermosillo, Sonora 83000, México 2Unidad Académica de Ciencias de la Tierra, Universidad Autónoma de Guerrero, A.P. 197, Taxco, Guerrero 40200, México 3Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA 4Departamento de Geología, Centro de Investigación Científi ca y de Educación Superior de Ensenada (CICESE), Km 107 Carr, Tijuana-Ensenada, Ensenada, Baja California, México We thank Keppie et al. (2008) for their com- the merger as a single group. In the following The youngest detrital zircon cluster in blue- ment that allows us to expand the discussion on sections, we answer each aspect discussed by schists (200–390 °C; 6–9 kbar) (Vega-Granillo the geology and metamorphic evolution of the Keppie et al. (2008) in their comment. et al., 2007) of the Ixcamilpa suite has a peak Acatlán Complex of southern Mexico. In our of ca. 477 Ma (U-Pb, zircon; Talavera-Mendoza paper (Vega-Granillo et al., 2007), we provide ONE OR THREE HP METAMORPHIC et al., 2005) indicating a maximum Early Ordo- geologic, petrologic, thermobarometric, and EVENTS IN THE ACATLÁN COMPLEX? vi cian depositional age. As indicated above, geo chronologic evidence of three distinctive the age of eclogitic metamorphism in the high-pressure (HP) metamorphic events of Early Three distinct HP metamorphic events are Xayacatlán suite predates that age. -
Diagnostico De La Condicion Y Posicion De Género De Las Mujeres En Epatlan, Puebla
DIAGNOSTICO DE LA CONDICION Y POSICION DE GÉNERO DE LAS MUJERES EN EPATLAN, PUEBLA DIAGNOSTICO DE LA CONDICION Y POSICION DE GÉNERO DE LAS MUJERES EN EPATLAN, PUEBLA DIAGNOSTICO DE LA CONDICION Y POSICION DE GÉNERO DE LAS MUJERES EN EPATLAN, PUEBLA “Este programa es público y queda prohibido su uso con fines partidistas o de promoción personal”. “Este programa es generado con recursos del Programa de Fortalecimiento a las Políticas Municipales de Igualdad y Equidad entre Mujeres y Hombres, FODEIMM”. [1] INDICE DE CONTENIDOS. 2 RESUMEN EJECUTIVO. 4 PRESENTACION. 5 INTRODUCCION. 6 OBJETIVOS. 8 CAP I MARCOS NORMATIVOS. 9 CAP II MARCO TEORICO METODOLOGICO. .13 CAP III ANALISIS DE GENERO: CONDICION Y POSICION. 15 “Este programa es público y queda prohibido su uso con fines partidistas o de promoción personal”. “Este programa es generado con recursos del Programa de Fortalecimiento a las Políticas Municipales de Igualdad y Equidad entre Mujeres y Hombres, FODEIMM”. [2] CAP IV ANALISIS: NECESIDADES E INTERES DE GÉNERO. .39 CAP V BRECHAS DE DESIGUALDAD. .46 CAP VI INDICADORES. .41 CAPVII SISTEMATIZACION DE RESULTADOS. 42 CONCLUSIONES Y ACUERDOS. 45 BIBLIOGRAFIA. .46 “Este programa es público y queda prohibido su uso con fines partidistas o de promoción personal”. “Este programa es generado con recursos del Programa de Fortalecimiento a las Políticas Municipales de Igualdad y Equidad entre Mujeres y Hombres, FODEIMM”. [3] RESUMEN EJECUTIVO Hoy en día la violencia de género, requiere un arduo trabajo desde la política pública a nivel federal, estatal, municipal e incluso en combinación de ellas, la importancia de un proyecto como IMM en Epatlán el cual requiere de la elaboración de un diagnóstico que permita a los responsables del proyecto y las instituciones benefactoras tener un conocimiento más amplio de las condiciones, sociales, económicas, políticas, ideológicas y culturales en los que se desenvuelve la mujer epátlense, con el objetivo de diseñar estrategias acordes a su realidad y contrarrestar la violencia de género. -
Crimson Tide Geonews
The newsletter of the Department of Geological Sciences in Crimson Tide The University of Alabama’s College of Arts & Sciences Box 870338 Tuscaloosa, Alabama 35487 www.geo.ua.edu GeoNews Spring 2010 A MESSAGE FROM THE NEW CHAIR: Ibrahim Çemen Alumni of geology departments nationwide are great supporters of their alma maters, and alumni of the UA Department of Geological Sciences are no exception. In fact, I find the alumni here more eager than usual to help the department. This is evidenced by the great success of the Geological Sciences Alumni Board (GSAB). How can an alumni and/or friend of DGS help? Scholarship support for undergraduate and graduate students is always needed to help attract and keep talented students in the department. The GSAB has long recognized this need and has provided $71,250.00 for scholarships since the initiation of the board in 2002. We also need your support to help with field trips, faculty travel and to bringing speakers to the campus for the colloquium series. In August 2009, after 25 years of service to the science of geology at Oklahoma State University, I One of our pressing needs is financial support to became the new Chair of the Department of Geological augment stipends for our Graduate Teaching Sciences at the University of Alabama. After four Assistantships. Our GTAs work very hard. They teach months in Tuscaloosa and a steep learning curve, I am three lab sections in comparison to two lab sections in just now beginning to settle in as the new Chair. most Ph.D. -
Petrogenesis and Tectonic Setting of the Peralkaline Pine Canyon Caldera, Trans-Pecos Texas, USA
Eastern Kentucky University Encompass EKU Faculty and Staff choS larship 10-2006 Petrogenesis and tectonic setting of the peralkaline Pine Canyon caldera, Trans-Pecos Texas, USA. John C. White Eastern Kentucky University, [email protected] Christian S. Benker Eastern Kentucky University Minghua Ren University of Texas at El Paso Kevin M. Urbanczyk Sul Ross State University Don W. Corrick Big Bend National Park Follow this and additional works at: http://encompass.eku.edu/fs_research Part of the Geology Commons, and the Tectonics and Structure Commons Recommended Citation White, J.C., Benker, S.C., Ren, M., Urbanczyk, K.M., and Corrick, D.W., 2006, Petrogenesis and tectonic setting of the peralkaline Pine Canyon caldera, Trans-Pecos Texas, USA. In: Peralkaline Rocks: A Special Issue Dedicated to Henning Sørensen, PERALK2005 Workshop (G. Markl, Ed.) Lithos, v. 91, p. 74-94. (doi: 10.1016.j.lithos.2006.03.015) This Article is brought to you for free and open access by Encompass. It has been accepted for inclusion in EKU Faculty and Staff choS larship by an authorized administrator of Encompass. For more information, please contact [email protected]. Lithos 91 (2006) 74–94 www.elsevier.com/locate/lithos Petrogenesis and tectonic setting of the peralkaline Pine Canyon caldera, Trans-Pecos Texas, USA ⁎ John Charles White a, , S. Christian Benker a, Minghua Ren b, Kevin M. Urbanczyk c, Donald W. Corrick d a Department of Earth Sciences, Eastern Kentucky University, Richmond, KY 40475, USA b Department of Geological Sciences, University of Texas at El Paso, El Paso, TX 79968, USA c Department of Earth and Physical Sciences, Sul Ross State University, Alpine, TX 79832, USA d National Park Service, Big Bend National Park, TX 79834, USA Received 4 July 2005; accepted 13 March 2006 Available online 19 May 2006 Abstract The Pine Canyon caldera is a small (6–7 km diameter) ash-flow caldera that erupted peralkaline quartz trachyte, rhyolite, and high-silica rhyolite lavas and ash-flow tuffs about 33–32 Ma. -
Birth and Evolution of the Rio Grande Fluvial
University of New Mexico UNM Digital Repository Earth and Planetary Sciences ETDs Electronic Theses and Dissertations Fall 9-21-2016 Birth and evolution of the Rio Grande fluvial system in the last 8 Ma:Progressive downward integration and interplay between tectonics, volcanism, climate, and river evolution Marisa N. Repasch Follow this and additional works at: https://digitalrepository.unm.edu/eps_etds Part of the Geology Commons, Geomorphology Commons, Hydrology Commons, Other Earth Sciences Commons, Sedimentology Commons, Tectonics and Structure Commons, and the Volcanology Commons Recommended Citation Repasch, Marisa N.. "Birth and evolution of the Rio Grande fluvial system in the last 8 Ma:Progressive downward integration and interplay between tectonics, volcanism, climate, and river evolution." (2016). https://digitalrepository.unm.edu/eps_etds/139 This Thesis is brought to you for free and open access by the Electronic Theses and Dissertations at UNM Digital Repository. It has been accepted for inclusion in Earth and Planetary Sciences ETDs by an authorized administrator of UNM Digital Repository. For more information, please contact [email protected]. Marisa Repasch Candidate Earth and Planetary Sciences Department This thesis is approved, and it is acceptable in quality and form for publication: Approved by the Thesis Committee: Karl Karlstrom Laura Crossey Matt Heizler i BIRTH AND EVOLUTION OF THE RIO GRANDE FLUVIAL SYSTEM IN THE LAST 8 MA: PROGRESSIVE DOWNWARD INTEGRATION AND INTERPLAY BETWEEN TECTONICS, VOLCANISM, CLIMATE, AND RIVER EVOLUTION BY MARISA REPASCH B.S. EARTH AND ENVIRONMENTAL SCIENCES LEHIGH UNIVERSITY 2014 M.S. THESIS Submitted in partial fulfillment of the Requirements for the Degree of Master of Science Earth and Planetary Sciences The University of New Mexico Albuquerque, New Mexico December, 2016 ii ACKNOWLEDGEMENTS First and foremost, I acknowledge my advisor, Karl Karlstrom, for all of the guidance, time, and energy he invested in my research, professional development, and personal well-being. -
Geologic Map of the Alamosa 30′ × 60′ Quadrangle, South-Central
Geologic Map of the Alamosa 30‘ × 60‘ Quadrangle, South-Central Colorado Scientific Investigations Map 3342 U.S. Department of the Interior U.S. Geological Survey Geologic Map of the Alamosa 30’ × 60’ Quadrangle, South-Central Colorado By Ren A. Thompson, Ralph R. Shroba, Michael N. Machette, Christopher J. Fridrich, Theodore R. Brandt, and Michael A. Cosca Scientific Investigations Map 3342 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2015 Supersedes Open-File Report 2005–1392, and Open-File Report 2008–1124 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 http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Thompson, R.A., Shroba, R.R., Machette, M.N., Fridrich, C.J., Brandt, T.R., and Cosca, M.A., 2015, Geologic map of the Alamosa 30’ × 60’ quadrangle, south-central Colorado: U.S. Geological Survey Scientific Investigations Map 3342, 23 p., scale 1:100,000, http://dx.doi.org/10.3133/sim3342.