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dc.contributor.author
Alvarez Pontoriero, Orlando
dc.contributor.author
Gimenez, Mario Ernesto
dc.contributor.author
Lince Klinger, Federico Gustavo
dc.contributor.author
Folguera Telichevsky, Andres
dc.contributor.author
Braitenberg, Carla
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Folguera Telichevsky, Andres
dc.contributor.other
Contreras Reyes, Eduardo
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Heredia, Nemesio
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Encinas, Alfonso
dc.contributor.other
Iannelli, Sofía
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Oliveros Clavijo, Veronica Laura
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Davila, Federico Miguel
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Collo, Gilda
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Giambiagi, Laura Beatriz
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Maksymowicz, Andrei
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Iglesia Llanos, Maria Paula
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Turienzo, Martin Miguel
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Naipauer, Maximiliano
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Orts, Darío Leandro
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Litvak, Vanesa Dafne
dc.contributor.other
Alvarez Pontoriero, Orlando
dc.contributor.other
Arriagada, César
dc.date.available
2020-06-02T18:46:23Z
dc.date.issued
2018
dc.identifier.citation
Alvarez Pontoriero, Orlando; Gimenez, Mario Ernesto; Lince Klinger, Federico Gustavo; Folguera Telichevsky, Andres; Braitenberg, Carla; The Peru-Chile Margin from Global Gravity Field Derivatives; Springer; 2018; 59-79
dc.identifier.isbn
978-3-319-67773-6
dc.identifier.uri
http://hdl.handle.net/11336/106518
dc.description.abstract
Deformation along the 3,500 km subduction Pacific margin of the Peru-Chile trench is partially controlled by ocean bathymetric heterogeneities and sediments. Oceanic highs (e.g. ridges, fracture zones, plateaus) influence deformation in the fore-arc zone where collision occurs, and control turbiditic flow dispersal and consequently the amount of sediments accreted at the frontal accretionary prism and subduction channel, compartmentalizing the trench into segments linked to seismic segmentation. Recent satellite missions (CHAMP, GRACE and GOCE) have introduced an extraordinary improvement in the reconstruction of the global gravity field. Earth gravity field models, mainly derived from satellite measurements, reflect mass inhomogeneities of the earth. This chapter focuses on the determination of mass heterogeneities over the oceanic plate and their relation to general distribution of sediments over the Peru-Chilean margin, seismic segmentation along the margin, and the relationship between trench sediment thickness and the variable Andean orogenic volume, by means of a gravimetric analysis. Using the gravity potential model EGM2008 and satellite GOCE data we calculated two functionals of the geopotential: the Bouguer anomaly and the vertical gravity gradient, both corrected for the topographic effect. The vertical gravity gradient field is of special interest as it highlights main geological features, and allows unraveling unknown structures that are concealed by sediments. From these, different features can be clearly depicted such as the contact between the Pacific oceanic crust and the South American plate, the Nazca Ridge, the Juan Fernandez Ridge and the Chile Rise, among others. The segmentation between a filled trench south of Juan Fernandez Ridge, a partially filled trench to the north up to the Copiapo Ridge, and a completely starved trench north of this latitude is depicted. Finally, the relationship between gravity derived fields, high oceanic features and seismic segmentation is discussed for the last megathrust earthquakes that affected this subductive plate boundary.
dc.format
application/pdf
dc.language.iso
eng
dc.publisher
Springer
dc.rights
info:eu-repo/semantics/restrictedAccess
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.subject
GRAVEDAD
dc.subject
TERREMOTOS
dc.subject.classification
Geología
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Ciencias de la Tierra y relacionadas con el Medio Ambiente
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CIENCIAS NATURALES Y EXACTAS
dc.title
The Peru-Chile Margin from Global Gravity Field Derivatives
dc.type
info:eu-repo/semantics/publishedVersion
dc.type
info:eu-repo/semantics/bookPart
dc.type
info:ar-repo/semantics/parte de libro
dc.date.updated
2020-02-19T20:21:25Z
dc.journal.pagination
59-79
dc.journal.pais
Alemania
dc.journal.ciudad
Berlín
dc.description.fil
Fil: Alvarez Pontoriero, Orlando. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales. Instituto Geofísico Sismológico Volponi; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
dc.description.fil
Fil: Gimenez, Mario Ernesto. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales. Instituto Geofísico Sismológico Volponi; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
dc.description.fil
Fil: Lince Klinger, Federico Gustavo. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales. Instituto Geofísico Sismológico Volponi; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
dc.description.fil
Fil: Folguera Telichevsky, Andres. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina
dc.description.fil
Fil: Braitenberg, Carla. Universita di Trieste; Italia
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/chapter/10.1007/978-3-319-67774-3_3
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/https://doi.org/10.1007/978-3-319-67774-3_3
dc.conicet.paginas
650
dc.source.titulo
The evolution of the Chilean-Argentinean Andes
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