Instituto Geológico y Minero de España

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Resultados de la consulta :
Instituto Geológico y Minero de España
 Registros del al 6 de 6 encontrados

1.-  Are the Taitao granites formed due to subduction of the Chile Ridge?
Elsevier; Amsterdam; NLD; Netherlands, 2009
Mantle dynamics and crust-mantle interactions in collisional orogens
Ver registro

2.-  Geochemical signature of amphibolite melting from ridge subduction-related granitoids; Chile Triple Junction area
Japan Geoscience Union; Tokyo; JPN; Japan, 2008
Abstract; Japanese Geoscience Union meeting 2008
Ver registro

3.-  Petrogenesis of the ridge subduction-related granitoids from the Taitao Peninsula, Chile Triple Junction area
Geochemical Society of Japan; Nagoya; JPN; Japan, 2013
Geoscience dynamics in the Patagonia Archipelago-Southern Pacific Ocean
Ver registro

4.-  Progressive metamorphism of the Taitao Ophiolite; evidence for axial and off-axis hydrothermal alterations
Elsevier; Amsterdam; NLD; Netherlands, 2007
Ver registro

5.-  Subduction of the Chile Ridge and generation of granite magmas
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2010
European Geosciences Union general assembly 2010
Ver registro

6.-  Tectonic and magmatic evolution of the Taitao Ophiolite and related granites, southern Chile
Geological Society of America (GSA); Boulder, CO; USA; United States, 2007
Geological Society of America, 2007 annual meeting
Ver registro


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