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Mantle Peridotite Xenoliths
Earth and Planetary Science Letters 260 (2007) 37–55 www.elsevier.com/locate/epsl Mantle peridotite xenoliths in andesite lava at El Peñon, central Mexican Volcanic Belt: Isotopic and trace element evidence for melting and metasomatism in the mantle wedge beneath an active arc ⁎ Samuel B. Mukasa a, , Dawnika L. Blatter b, Alexandre V. Andronikov a a Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109-1005, USA b Department of Earth and Planetary Science, University of California, Berkeley, CA 94720, USA Received 6 July 2006; received in revised form 3 May 2007; accepted 7 May 2007 Available online 13 May 2007 Editor: R.W. Carlson Abstract Peridotites in the mantle wedge and components added to them from the subducting slab are thought to be the source of most arc magmas. However, direct sampling of these materials, which provides a glimpse into the upper mantle beneath an active margin, is exceedingly rare. In the few arc localities where found, peridotite xenoliths are usually brought to the surface by basaltic magmas. Remarkably, the hornblende-bearing ultramafic xenoliths and clinopyroxene megaxenocrysts from El Peñon in the central Mexican Volcanic Belt were brought to the surface by a Quaternary high-Mg siliceous andesite, a rock type usually considered too evolved to be a direct product of mantle melting. The xenoliths and megaxenocrysts from El Peñon represent lithospheric mantle affected by significant subduction of oceanic lithosphere since as early as the Permian. Trace element and radiogenic isotope data we report here on these materials suggest a history of depletion by melt extraction, metasomatism involving a fluid phase, and finally, limited reaction between the ultramafic materials and the host andesite, probably during transport. -
Article in Press + Model
ARTICLE IN PRESS + MODEL Journal of Volcanology and Geothermal Research xx (2006) xxx–xxx www.elsevier.com/locate/jvolgeores The 1968 andesitic lateral blast eruption at Arenal volcano, Costa Rica ⁎ Guillermo E. Alvarado a, , Gerardo J. Soto a, Hans-Ulrich Schmincke b, Louise L. Bolge c, Mari Sumita b a Observatorio Sismológico y Vulcanológico de Arenal y Miravalles (OSIVAM), Instituto Costarricense de Electricidad (ICE), Apdo. 10032-1000, Costa Rica b SFB 574, University of Kiel and Leibniz Institute for Marine Science (IFM-Geomar), Wischhofstrasse 1-3, 24148 Kiel, Germany c Boston University, Department Earth Sciences, 685 Commonwealth Ave., Boston, MA 02215, USA Received 6 June 2005; accepted 28 March 2006 Abstract The magmatic andesitic eruption of Arenal volcano on July 29–31, 1968, after centuries of dormancy, produced three new fissural craters (A, B and C) on its western flank and a multilayered pyroclastic deposit emplaced by complex transport mechanisms. The explosions were initially triggered by a volatile oversaturated (4–7 wt.% H2O) magma. Several lines of evidences suggest a small blast surge, where a wood-rich pyroclastic deposit was emplaced as a ground layer, followed by several units of coarse-grained (MdΦ between −0.65 and −5.40) tephra deposits (LU: lapilli units, DAU: double ash units). LU-1, -2, -3, DAU-1 and -2 consist of unconsolidated and well- to poorly sorted vesiculated bombs and lapilli of andesite, some blocks, ash and shredded wood. The individual units are possibly correlated with the major explosions of July 29. The thickness of the deposits decreases with the distance from the volcano from 5.6 m to a few centimeters. -
Elaboración De Cartografía Geológica Y Geomorfológica De Cinco Subcuencas De La Parte Alta De La Cuenca Alta Del Río Nahualate
ELABORACIÓN DE CARTOGRAFÍA GEOLÓGICA Y GEOMORFOLÓGICA DE CINCO SUBCUENCAS DE LA PARTE ALTA DE LA CUENCA ALTA DEL RÍO NAHUALATE María Mildred Moncada Vásquez Marzo 16, 2017 ÍNDICE 1. INTRODUCCIÓN ...................................................................................................................................... 6 2. OBJETIVOS .............................................................................................................................................. 7 3. ANTECEDENTES ...................................................................................................................................... 7 4. ENCUADRE TECTÓNICO REGIONAL ........................................................................................................ 9 5. CONTEXTO VOLCÁNICO REGIONAL ......................................................................................................10 6. METODOLOGÍA .....................................................................................................................................12 7. CARTOGRAFÍA GEOLÓGICA ..................................................................................................................16 7.1 Procesos y unidades litológicas asociadas a Calderas Atitlán ......................................................16 7.1.1 Rocas graníticas (Tb - Tbg) ..........................................................................................................16 7.1.2 Toba María Tecún (Tmt) .....................................................................................................20 -
Arenal Volcano Tours
TRUST THE EXPERTS Hand Crafted Itineraries Curated Hotel Collection Luxury Vehicles Experienced Travel Consultants ARENAL VOLCANO 24/7 In-Country TOURS Assistance The Arenal Volcano once erupted an average of 41 times per day. Today, the volcano is in a resting phase but still a sight to behold. The region is not only home to the volcano, it also benefits from volcano-fed thermal hot springs, plunging waterfalls, the impressive Over 50,000 Satisfied size of Lake Arenal, and a rich secondary rainforest ecosystem with Customers exotic wildlife. Now considered by many the adventure capital of Costa Rica, Arenal is a great base for adventure tours like zip-lining, whitewater rafting, COSTA RICA waterfall rappelling, and more. EXPERTS The listed tours are available from hotels in the central Arenal zone. 3166 N Lincoln Ave., Additional fees may apply for hotels outside of the central zone Suite 424 Chicago, IL. 60657 www.costaricaexperts.com Phone: 800-827-9046 Fax: 773-935-9252 Arenal Hanging Bridges Hike Hike across the Arenal Hanging Bridges with a naturalist guide for a perfect half-day Arenal tour. This ecotourism project of solid ground trails and state of the art hanging bridges was designed for the observation and conservation of Costa Rica’s incredible nature. The reserve, with nearly 370 acres of rainforest, is home to countless species of amazing birds, mammals, and lush vegetation. You will walk along the treetops with your naturalist guide, encountering 8 fixed bridges and 6 hanging bridges. These connect gaps in the reserve canyon, allowing you to walk right into the most important layers of the rainforest. -
Una Teorãła Sobre El Origen De Los Peces De Xiloã€
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Investigations of the Ichthyofauna of Nicaraguan Lakes Papers in the Biological Sciences 1976 Una teoría sobre el origen de los peces de Xiloà Jaime Villa Cornell University Follow this and additional works at: https://digitalcommons.unl.edu/ichthynicar Part of the Aquaculture and Fisheries Commons Villa, Jaime, "Una teoría sobre el origen de los peces de Xiloà" (1976). Investigations of the Ichthyofauna of Nicaraguan Lakes. 12. https://digitalcommons.unl.edu/ichthynicar/12 This Article is brought to you for free and open access by the Papers in the Biological Sciences at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Investigations of the Ichthyofauna of Nicaraguan Lakes by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Published in INVESTIGATIONS OF THE ICHTHYOFAUNA OF NICARAGUAN LAKES, ed. Thomas B. Thorson (University of Nebraska-Lincoln, 1976). Copyright © 1976 School of Life Sciences, University of Nebraska-Lincoln. Reprinted from ENCUENTRO: REv. UNIV. CENTROAMERICANA 1(4):202-214, July-Aug., 1968. J.lme VIII. Una leoria sobre el orlgen• de los peces de Xiloa 1.- INTRODUCCION A finales de 1965 v en conexion con estudios en curso sobre la herpetolo g(a nicaragiiense colec te una pequena serie de peces de la Laguna de Xiloa que revela- ron aspectos interesantes y me indujeron a realizar colecciones extensivas en toda la laguna; estas colecciones se realizaron durante 1966-68 y cons tan de varios cien tos de ejemplares, depositados en la Universidad de Costa Rica y en mi coleccion particular. El material acumulado durante estos anos y las notas tomadas durante todo el tiempo en que se realizaron han sido suficientes para permitir una serie de conclusiones en diversos aspectos, algunas de las cuales han sido ya publicadas 0 se encuentran en preparacion. -
Supply for H Cement
REQUEST OF PROPOSAL FOR EXPRESSION OF INTEREST – SUPPLY OF CLASS H CEMENT. Introduction LaGEO S.A. de C.V. (LAGEO), a power production company of El Salvador, is in the final stages of negotiating a loan with the World Bank (P170089 – financial identifier of the project within the World Bank) to increase the generation of electrical energy based on local geothermal resources. The scope of the project consists of the construction and commissioning of two condensing geothermal plants, one to be installed in the Chinameca geothermal field in eastern El Salvador with a generation capacity of 25 MW and the other to be placed in the San Vicente geothermal field in central El Salvador with a generation capacity of 10 MW. A vital component of these projects is drilling additional geothermal wells, which require the supply of Class H cement supply. This expression of interest request aims to understand the market for the specific requirement for the supply of Class H cement for a total of nine (9) wells in the Chinameca and San Vicente geothermal fields. Likewise, establish communication with interested companies, who will subsequently be informed about the tender process and invited to participate in it. Project Description Chinameca Geothermal Field The Chinameca geothermal field is located 130 km east of San Salvador, the capital city of El Salvador, in the department of San Miguel, within the Pacayal-Limbo volcanic complex. The towns of Chinameca and Nueva Guadalupe, both located to the north of the geothermal field. The supply of Class H cement will be used to drill six (6) geothermal wells. -
Mejoras En El Paradigma Del Manejo De La Gestión Del Riesgo En Los Parques Nacionales Volcánicos De Costa Rica, Entre El Año 2000 Y El 2020
Revista Geológica de América Central, 64, 1-15 , 2021 doi: 10.15517/rgac.v0i64.46615 ISSN: 0256-7024 Mejoras en el paradigma del manejo de la gestión del riesgo en los parques nacionales volcánicos de Costa Rica, entre el año 2000 y el 2020 Improvements in risk management paradigm in Costa Rican volcanic national parks between 2000 and 2020 Guillermo E. Alvarado*, Lidier Esquivel y Blas Sánchez Comisión Nacional de Prevención de Riesgos y Atención de Emergencias (CNE), Unidad de Investigación y Análisis del Riesgo, San José, Costa Rica *Autor para contacto: [email protected] (Recibido: 23/08/2020; aceptado 13/01/2021) RESUMEN: Costa Rica es conocida a nivel mundial como una meca turística. A partir de 1955, casi todos los grandes volcanes comenzaron a ser declarados parques nacionales, deteniendo la ocupación y explotación humana en la cúspide de estos sectores, al tiempo que varios parques han estado expuestos a la actividad eruptiva de los cinco volcanes históricamente activos. Los parques nacionales volcánicos están sujetos al turismo y, con ello, al peligro de que se puedan generar afectación y pérdidas en vidas huma- nas. La muerte de una turista norteamericana y su guía costarricense en el año 2000, así como la repentina erupción del Poás en el año 2017, aunado a la persistente actividad eruptiva del Turrialba por más de 10 años, fueron los mecanismos disparadores de cuatro grandes cambios en el manejo y seguridad de los parques volcánicos costarricenses: a) la generación del decreto de restricción del uso de la tierra alrededor -
Amenaza Volcánica Del Área De Managua Y Sus Alrededores (Nicaragua)”
Parte II.3: Amenaza volcánica 127 Parte II.3 Guía técnica de la elaboración del mapa de “Amenaza volcánica del área de Managua y sus alrededores (Nicaragua)” 128 Parte II.3: Amenaza volcánica Índice 1 Resumen.......................................................................................................................130 2 Lista de figuras y tablas...............................................................................................131 3 Introducción.................................................................................................................132 4 Objetivos.......................................................................................................................132 5 Metodología.................................................................................................................133 5.1 Recopilación de los datos y análisis de los peligros volcánicos existentes............133 5.1.1 Complejo Masaya.............................................................................................133 5.1.1.1 Flujos de lava..............................................................................................134 5.1.1.2 Caída de tefra..............................................................................................134 5.1.1.3 Flujos piroclásticos y Oleadas piroclásticas...............................................135 5.1.1.4 Flujos de lodo y detritos (lahares)..............................................................135 5.1.1.5 Emanaciones de gas....................................................................................136 -
Chemical and Isotopic Studies of Monogenetic Volcanic Fields: Implications for Petrogenesis and Mantle Source Heterogeneity
MIAMI UNIVERSITY The Graduate School Certificate for Approving the Dissertation We hereby approve the Dissertation of Christine Rasoazanamparany Candidate for the Degree DOCTOR OF PHILOSOPHY ______________________________________ Elisabeth Widom, Director ______________________________________ William K. Hart, Reader ______________________________________ Mike R. Brudzinski, Reader ______________________________________ Marie-Noelle Guilbaud, Reader ______________________________________ Hong Wang, Graduate School Representative ABSTRACT CHEMICAL AND ISOTOPIC STUDIES OF MONOGENETIC VOLCANIC FIELDS: IMPLICATIONS FOR PETROGENESIS AND MANTLE SOURCE HETEROGENEITY by Christine Rasoazanamparany The primary goal of this dissertation was to investigate the petrogenetic processes operating in young, monogenetic volcanic systems in diverse tectonic settings, through detailed field studies, elemental analysis, and Sr-Nd-Pb-Hf-Os-O isotopic compositions. The targeted study areas include the Lunar Crater Volcanic Field, Nevada, an area of relatively recent volcanism within the Basin and Range province; and the Michoacán and Sierra Chichinautzin Volcanic Fields in the Trans-Mexican Volcanic Belt, which are linked to modern subduction. In these studies, key questions include (1) the role of crustal assimilation vs. mantle source enrichment in producing chemical and isotopic heterogeneity in the eruptive products, (2) the origin of the mantle heterogeneity, and (3) the cause of spatial-temporal variability in the sources of magmatism. In all three studies it was shown that there is significant compositional variability within individual volcanoes and/or across the volcanic field that cannot be attributed to assimilation of crust during magmatic differentiation, but instead is attributed to mantle source heterogeneity. In the first study, which focused on the Lunar Crater Volcanic Field, it was further shown that the mantle heterogeneity is formed by ancient crustal recycling plus contribution from hydrous fluid related to subsequent subduction. -
Geohazard Supersites and Natural Laboratories Initiative
Versión 1.0, 14 de octubre de 2015 www.earthobservations.org/gsnl.php Geohazard Supersites and Natural Laboratories Initiative A.1 Proposal Title: Volcano-tectonic Geohazard Interaction within the Nicaraguan Depression Volcanoes: Cosiguina, San Cristóbal, Telica, Cerro Negro, Momotombo, Península de Chiltepe, Masaya and Concepción A.2 Supersite Coordinator Email (Organization only) [email protected] Name: Iris Valeria Surname: Cruz Martínez Position: Director General of Geology and Geophysics Personal website: <In case a personal web page does not exist, please provide a CV below this table> Institución: Instituto Nicaragüense de Estudios Territoriales-INETER- Nicaragua Type of institution Government (Government, Education, other): The institution's web address: https://www.ineter.gob.ni/ Address: Front of Solidarity Hospital City: Managua Postal Code/Postal Code: 2110 Managua, Nicaragua Country: Nicaragua Province, Territory, State or Managua County: Phone number: Tel. +505-22492761 Fax +505-22491082 1 Versión 1.0, 14 de octubre de 2015 A.3 Core Supersite Team Email (Organization only) [email protected] Name: Federico Vladimir Surname: Gutiérrez Corea Position: Director of the Nicaraguan Institute of Territorial Studies-INETER- Nicaragua Personal website: http://www.vlado.es/ http://uni.academia.edu/FedericoVLADIMIRGutierrez/Curriculu mVitae Institution: Nicaraguan Institute of Territorial Studies-INETER-Nicaragua Type of institution Government (Government, Education, others): Institution's web address: https://www.ineter.gob.ni/ -
La Fortuna Travel Guide
La Fortuna Travel Guide Coherent and soli Marv often soliloquising some harassment uncannily or cocoons rallentando. Dichroscopic Ernst coalescing his Clermont-Ferrand beeswax darkly. Nymphomania and relational Agamemnon typings her totalisers galls or creolizing bitter. This place with luxury on la fortuna If he do bargain to naked up this goal anyway, exercise obedience and respect the area. Yes, there is half for everyone here. Just freight in the Observatory and the roadside would find happy and provide directions. We grieve along swift river at about another hour, rule which white spot turtles lying out at the banks to collaborate some saw, a completely unexpected river otter playing in wine water, and with second sloth of river trip. It is whether simple to soon to La Fortuna, and there art a host different options. It team be difficult to decide, under a refrigerator, which hotel will better meet your requirements, which and why, at Costa Rica Rios, we bake here well help you. Set tube in the Costa Rican rain forests, Sarapiquà River, declared as Nation. Specific Costa Rican creatures you depart look forward go seeing include iguanas, coati mundi, and colorful toucans. Lake Arenal to the divide, and the Cano Negro Wildlife head to convince north. Uber will amplify available complicate the return them by changing your pickup point. Arenal region, Costa Rica. How was able visit? La Paz Waterfall Gardens for breathtaking scenery and lots of photo opps! Never find new blog posts and receive LE Travels monthly newsletter by subscribing below. Your password was changed successfully. But offspring are a number of waterfalls and canyons here. -
Estudio Técnico De Linea Base Del Complejo Volcánico Acatenango - Fuego
ESTUDIO TÉCNICO DE LINEA BASE DEL COMPLEJO VOLCÁNICO ACATENANGO - FUEGO Índice I. EQUIPO TECNICO .....................................................................................................................1 II. RESUMEN EJECUTIVO ...........................................................................................................2 III. ANTECEDENTES.....................................................................................................................3 IV. METODOLOGÍA ......................................................................................................................5 V. CARACTERIZACION DEL ÁREA ........................................................................................10 VI. ACTIVIDADES POTENCIALES ..........................................................................................48 VII. DEFINICIÓN DE OBJETOS DE CONSERVACIÓN ........................................................49 VIII. CONCLUSIONES ................................................................................................................51 IX. RECOMENDACIONES ..........................................................................................................51 X. BIBLIOGRAFIA .......................................................................................................................53 XI. ANEXOS ..................................................................................................................................57 ÍNDICE DE FIGURAS Y CUADROS Figura 1. Delimitación del