| Registros del 1 al 10 de 26 encontrados |
1.- A LAURENTIAN? GRENVILLE-AGE OCEANIC ARC/BACK-ARC TERRANE IN THE SIERRA DE PIE DE PALO, WESTERN SIERRAS PAMPEANAS, ARGENTINA
GEOLOGICAL SOCIETY OF LONDON; LONDON; GBR; UNITED KINGDOM, 1998
THE PROTO-ANDEAN MARGIN OF GONDWANA
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2.- Andean adakite-like high-Mg andesites on the northern margin of the Chilean-Pampean flat-slab (27-28.5 degrees S) associated with frontal arc migration and fore-arc subduction erosion
Oxford University Press; Oxford; GBR; United Kingdom, 2013
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3.- ANDEAN ADAKITES FROM MELTING OF SUBDUCTED SLABS, THICKENED CONTINENTAL CRUST, AND TECTONICALLY REMOVED FOREARC AND BACKARC CRUST
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2000
AGU 2000 FALL MEETING
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4.- CENTRAL ANDEAN ORE DEPOSITS LINKED TO EVOLVING SHALLOW SUBDUCTION SYSTEMS AND THICKENING CRUST
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2001
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5.- Chemical and isotopic evidence for modification of the Central Andean Arc mantle by crust removed by forearc subduction erosion
Pergamon; Oxford; III; International, 2006
Abstracts of the 16th annual V. M. Goldschmidt conference
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6.- CRUSTAL RECYCLING
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 1998
GEOLOGICAL SOCIETY OF AMERICA, 1998 ANNUAL MEETING
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7.- Early to middle Miocene backarc magmas of the Neuquen Basin; geochemical consequences of slab shallowing and the westward drift of South America
Geological Society of America (GSA); Boulder, CO; USA; United States, 2006
Evolution of an Andean margin; a tectonic and magmatic view from the Andes to the Neuquen Basin (35 degrees -39 degrees S lat)
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8.- EPISODIC ARC MIGRATION, CRUSTAL THICKENING, SUBDUCTION EROSION, AND MAGMATISM IN THE SOUTH-CENTRAL ANDES
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2005
Ver registro
9.- Evolution of an Andean margin; a tectonic and magmatic view from the Andes to the Neuquen Basin (35 degrees -39 degrees S lat)
Geological Society of America (GSA); Boulder, CO; USA; United States, 2006
Ver registro
10.- Evolution of the late Miocene Chachahuen volcanic complex at 37 degrees S over a transient shallow subduction zone under the Neuquen Andes
Geological Society of America (GSA); Boulder, CO; USA; United States, 2006
Evolution of an Andean margin; a tectonic and magmatic view from the Andes to the Neuquen Basin (35 degrees -39 degrees S lat)
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