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A Farewell to Peter Coneylegacy of Great Teaching, a Legacy of How Things Are Done in a Collaborative Spirit
UA Geosciences Newsletter, Volume 4, Number 2 (Spring 1999) Item Type Newsletter Authors University of Arizona Department of Geosciences Publisher Department of Geosciences, University of Arizona (Tucson, AZ) Rights Copyright © Arizona Board of Regents. The University of Arizona. Download date 26/09/2021 18:13:55 Link to Item http://hdl.handle.net/10150/295174 THE UNIVERSITYOF ARIZONA® The Department of Geosciences Spring 1999 . Volume 4, Number 2 Letter from the Chair Joaquin Ruiz Peter Coney's untimely death is the Department's sad news. In 1982 I read an ad in EOS describing a job opening at The University of Arizona.I had just finished my PhD dissertation on the origin of tin -rich rhyolites of the Sierra Madre Occidental in Mexico and had based many of my conclusions on Peter Coney's suspect terrane map of Mexico and his ideas of magmatism in the western US. I could barely wait to meet this scientist. His papers were imaginative and thought provoking. Of course, the papers reflected the man. After I got to know Peter, I was also struck by his humanity. Peter cared about people. He deeply cared for his students and was able to transmit to them his knowledge, his analysis and his calm. In fact, what made Peter such a remarkable individual Peter Coney in the northern Snake Range detachment fault. (photo by Peter DeCelles) was his genius combined with his humanity. Peter left us with many legacies -a legacy of great thinking of how the Earth works, a A Farewell to Peter Coneylegacy of great teaching, a legacy of how things are done in a collaborative spirit. -
Geologic Resources Inventory Report
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Tumacácori National Historical Park Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2011/439 ON THE COVER A rainbow over Mission San José de Tumacácori, one of three missions within Tumacácori National Historical Park. National Park Service photograph by Ed Wittenberg. THIS PAGE Tumacacori Peak looms over Mission San José de Tumacácori in this view to the west. National Park Service photograph. Photographs courtesy Jeremy Moss (Tumacácori NHP) Tumacácori National Historical Park Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2011/439 National Park Service Geologic Resources Division PO Box 25287 Denver, CO 80225 August 2011 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado publishes a range of reports that address natural resource topics of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. -
Colombian Geothermal Resources
Proceedings World Geothermal Congress 2005 Antalya, Turkey, 24-29 April 2005 Colombian Geothermal Resources Claudia Alfaro*1, Francisco Velandia*2 and Héctor Cepeda*3 * INGEOMINAS. Dg. 53 No. 34-53. Bogotá, Colombia 1 [email protected] , 2 [email protected], 3 [email protected] Keywords: Colombia, Nevado del Ruiz, Paipa, Azufral, electromagnetic surveys and geochemistry of the aqueous structural geology of Paipa, vulcanism at the Eastern phase of the hot springs. From them a high temperature Cordillera, geochemistry of hot springs. geothermal system is proposed with a magmatic heat source, an upflow controlled by deep faults and a shallow ABSTRACT mixing process with a highly sodium sulfate mineralized water which “masks” the chemical composition of the deep During the last few years, new legal dispositions have reservoir fluid. favored the promotion of non-conventional energy sources in Colombia: The law 697 of 2001 declared the rational and efficient use of energy and the utilization of non- 1. INTRODUCTION conventional energy sources, as a social and public interest Between 2000 and 2005, new legal dispositions have matter as well as a national convenience issue. The same favored the promotion of non-conventional energy sources law, demands stimulus for developing non-conventional in Colombia. The law 697 of 2001 declared the rational and energy sources from the government. The edict 3683 dated efficient use of energy and the utilization of non- December 2003, regulates the promotion of non- conventional energy sources, as a social and public interest conventional energy sources, inside the frame of sustainable matter as well as a national convenience issue. -
Paipa Geothermal System, Boyacá
Volume 4 Quaternary Chapter 4 Neogene https://doi.org/10.32685/pub.esp.38.2019.04 Paipa Geothermal System, Boyacá: Review Published online 20 May 2020 of Exploration Studies and Conceptual Model Paleogene Claudia María ALFARO–VALERO1* , Jesús Bernardo RUEDA–GUTIÉRREZ2 , 3 4 Jhon Camilo MATIZ–LEÓN , Miguel Angel BELTRÁN–LUQUE , 1 [email protected] 5 6 Gilbert Fabián RODRÍGUEZ–RODRÍGUEZ , Gina Z. RODRÍGUEZ–OSPINA , Servicio Geológico Colombiano 7 8 Dirección de Geociencias Básicas Carlos Eduardo GONZÁLEZ–IDÁRRAGA , and Jaison Elías MALO–LÁZARO Diagonal 53 n.° 34–53 Cretaceous Bogotá, Colombia Abstract The Paipa geothermal system is located at 2525 masl in a terrain tilted from 2 [email protected] Servicio Geológico Colombiano south to north towards the Chicamocha River, where the geology is dominated by Dirección de Geociencias Básicas sedimentary rocks intruded by felsic magmas. The Miocene and Pleistocene volcanic Diagonal 53 n.° 34–53 Bogotá, Colombia activity produced pyroclastic deposits and dome complexes. A deep saline sodium Jurassic 3 [email protected] sulfate water, presumably originating from the infiltration of meteoric water followed Servicio Geológico Colombiano Dirección de Geociencias Básicas by dissolution of an evaporite, mixes with geothermal fluid. This process masks the Diagonal 53 n.° 34–53 chemical and isotopic composition of the geothermal component of fluid discharge in Bogotá, Colombia 4 [email protected] hot springs, the temperatures of which reach 76 °C. Organic and magmatic/mantle con- Servicio Geológico Colombiano Triassic tributions also affect the composition of the gas phase discharges. High concentrations Dirección de Geociencias Básicas Diagonal 53 n.° 34–53 of radioactive elements are found in the area, mainly in El Durazno Intrusive, a highly Bogotá, Colombia altered intrusion located to the west. -
Experiment Number Short Name LONG NAME FDSN SEED Years
Experiment Number Short Name LONG NAME FDSN SEED years FDSN ID/ASSEMBLED % Data Available Experiment Status POOL TYPE PI Institution Start End Source Archiving format # instruments 8601 Ouachita 1986 OUACHITA Lithospheric Seismology Experiment (OUACHITA) 87-001 NA -completed archived PASSCAL Keller UTEP 5/2/90 6/1/90 Active SEGY 8602 Basin & Range Active PASSCAL Basin and Range Lithospheric Seismic Experiment, Northern Nevada (NEVADA) 00-029 NA -completed archived PASSCAL Thompson Stanford 6/2/90 7/2/90 Active SEGY 8801 Basin & Range Passive Passcal Basin and Range Passive-Source Seismic Exp. Part1: Lg Aperature Array Data (BRE1) 90-001 & 002 NA -completed archived PASSCAL Owens U of Mo 8/2/92 6/1/93 Passive SEED 1 8802 Brooks Range Pilot 1988 PASSCAL Brooks Range Seismic Survey (BROOKS) 92-001 NA -completed archived PASSCAL Levander Rice 7/2/92 8/16/92 Active SEGY 1 8901 APT 1989 Archean-Proterozoic transition Experiment (APT) 91-003 NA -completed archived PASSCAL Silver Carnegie 5/2/93 10/2/93 Passive SEED 6 8902 Greenland 1989 Greenland Seismic Survey 1989 Greenland Seismic Survey (GRN89) 94-005 NA -completed archived PASSCAL Smithson University of Wyoming 9/2/93 10/2/93 Active SEGY 35 8903 Loma Prieta RAMP Loma Prieta Aftershock Earthquake Dataset (LPF) 90-008 NA -completed archived PASSCAL Lerner-Lam Lamont 10/6/93 1/1/94 Passive SEED 1 9001 KRISP 90 Kenya Rift International Seismic Project (KRISP) 1990 (KRSP90) 03-002 NA -completed archived PASSCAL Meyer Wisconsin 1/2/94 4/16/94 Passive SEED 15 9003 Beaufort Sea 1990 Beaufort Ambient -
Map and Database of Quaternary Faults and Folds in Colombia and Its Offshore Regions
U.S. Department of the Interior U.S. Geological Survey Map and Database of Quaternary Faults and Folds in Colombia and its Offshore Regions By Gabriel Paris, Michael N. Machette, Richard L. Dart, and Kathleen M. Haller Open-File Report 00-0284 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards nor with the North American Stratigraphic Code. Any use of trade names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey. 2000 MAP AND DATABASE OF QUATERNARY FAULTS AND FOLDS IN COLOMBIA AND ITS OFFSHORE REGIONS A project of the International Lithosphere Program Task Group II-2, Major Active Faults of the World Data and map compiled by 1 GABRIEL PARIS, 2 MICHAEL N. MACHETTE, 2 RICHARD L. DART, AND 2 KATHLEEN M. HALLER 1 Departamento de Geografia Universidad del Valle Melendez, Cali, Colombia 2 U.S. Geological Survey (USGS) Central Geologic Hazards Team MS 966, P.O. Box 25046 Denver, Colorado, USA Regional Coordinator for South America CARLOS COSTA Universidad Nacional de San Luis Departmento de Geologia Casilla de Correo 320 San Luis, Argentina ILP Task Group II-2 Co-Chairman, Western Hemisphere MICHAEL N. MACHETTE U.S. Geological Survey (USGS) Central Geologic Hazards Team MS 966, P.O. Box 25046 Denver, Colorado, USA May 2000 version International Lithosphere Program i TABLE OF CONTENTS Page INTRODUCTION.................................................................................................................................1 -
Views of My Manuscript Greatly Improved It
University of Alberta Geochronology, Petrography, Geochemical Constraints, and Fluid Characterization of the Buriticá Gold Deposit, Antioquia Department, Colombia. by Guillaume Lesage A thesis submitted to the Faculty of Graduate Studies and Research in partial fulfillment of the requirements for the degree of Master of Science Earth and Atmospheric Sciences ©Guillaume Lesage Fall, 2011 Edmonton, Alberta Permission is hereby granted to the University of Alberta Libraries to reproduce single copies of this thesis and to lend or sell such copies for private, scholarly or scientific research purposes only. Where the thesis is converted to, or otherwise made available in digital form, the University of Alberta will advise potential users of the thesis of these terms. The author reserves all other publication and other rights in association with the copyright in the thesis and, except as herein before provided, neither the thesis nor any substantial portion thereof may be printed or otherwise reproduced in any material form whatsoever without the author’s prior written permission. Abstract Buriticá is a low- to intermediate-sulfidation epithermal gold deposit located 75 km north of Medellín, in Colombia. It is hosted by the Buriticá andesite porphyry, a shallow intrusive rock dated at 7.41 ± 0.40 Ma (40Ar/39Ar on hornblende), which intrudes the Cretaceous Cañasgordas Group and Buriticá stock. Gold mineralization is associated with a proximal sericite-adularia and a distal epidote-rich propylitic alteration, and is hosted in two different sets of veins respectively striking and dipping around 072°/87°S and 105°/87°S. Hydrothermal sericite yields an age of 7.74 ± 0.08 Ma. -
Structure and Age of the Lower Magdalena Valley
Journal of South American Earth Sciences 74 (2017) 1e26 Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames Structure and age of the Lower Magdalena Valley basin basement, northern Colombia: New reflection-seismic and U-Pb-Hf insights into the termination of the central andes against the Caribbean basin J. Alejandro Mora-Bohorquez a, *, Mauricio Ibanez-Mejia b, c, Onno Oncken d, Mario de Freitas e, Vickye Velez a, Andres Mesa f, Lina Serna a a Hocol S.A., Cra 7 No. 113-46, 16th Floor, Bogota, Colombia b Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA c Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA d Deutsches GeoForschungsZentrum GFZ, Telegranfenberg 14473, Potsdam, Germany e Caravela Energy, Bogota, Colombia f Horizonz Consulting, Bogota, Colombia article info abstract Article history: Detailed interpretations of reflection seismic data and new U-Pb and Hf isotope geochemistry in zircon, Received 8 July 2016 reveal that the basement of the Lower Magdalena Valley basin is the northward continuation of the Received in revised form basement terranes of the northern Central Cordillera, and thus that the Lower Magdalena experienced a 19 December 2016 similar pre-Cenozoic tectonic history as the latter. New U-Pb and Hf analyses of zircon from borehole Accepted 3 January 2017 basement samples retrieved in the basin show that the southeastern region consists of Permo-Triassic Available online 3 January 2017 (232-300Ma) metasediments, which were intruded by Late Cretaceous (75e89 Ma) granitoids.