The Hudson Volcano and surrounding monogenetic centres (Chilean Patagonia): An example of volcanism associated with ridge–trench collision environment
Authors:
- F. GutiérrezF. Gutiérrez
- A. GioncadaA. Gioncada
- O. González FerranOFO. González Ferran
- A. LahsenALA. Lahsen
- R. MazzuoliRMR. Mazzuoli
- 1 July 2005
- journal article
- Published by Elsevier in Journal of Volcanology and Geothermal Research
- Vol. 145 (3-4) , 207-233
Abstract
No abstract availableKeywords
This publication has 33 references indexed in Scilit:
- Quaternary volcanic activity of Hudson and Lautaro volcanoes, Chilean Patagonia: New constraints from K-Ar agesRevista geológica de Chile, 2004
- Magmatic–tectonic effects of high thermal regime at the site of active ridge subduction: the Chile Triple Junction modelTectonophysics, 2000
- The Pali Aike Volcanic Field, Patagonia: slab-window magmatism near the tip of South AmericaTectonophysics, 2000
- New geochemical constraints for the origin of ridge-subduction-related plutonic and volcanic suites from the Chile Triple Junction (Taitao Peninsula and Site 862, LEG ODP141 on the Taitao Ridge)Tectonophysics, 1999
- Holocene explosive activity of Hudson Volcano, southern AndesBulletin of Volcanology, 1998
- Neogene Patagonian plateau lavas: Continental magmas associated with ridge collision at the Chile Triple JunctionTectonics, 1997
- The Liquiñe Ofqui fault zone: a long-lived intra-arc fault system in southern ChileTectonophysics, 1996
- Postseismic coastal uplift in southern ChileGeophysical Research Letters, 1992
- Southern Patagonian plateau basalts and deformation: Backarc testimony of ridge collisionsTectonophysics, 1992
- Geological manifestations of ridge collision: Evidence from the Golfo de Penas‐Taitao Basin, southern ChileTectonics, 1985