Orogen‐Parallel Transition From a Decoupled Fore‐Arc Sliver to Andean‐Type Mountain Chain: Paleomagnetic and Geologic Evidence From Southern Chile (37–39°S)
Author:
Affiliation:
1. Istituto Nazionale di Geofisica e Vulcanologia Rome Italy
2. Now at Tecnologias Avanzadas Inspiralia SL Madrid Spain
3. Now at Scripps Institution of Oceanography La Jolla CA USA
Funder
Istituto Nazionale di Geofisica e Vulcanologia
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019TC005881
Reference103 articles.
1. Postmagmatic cooling and late Cenozoic denudation of the North Patagonian Batholith in the Los Lagos region of Chile, 41°−42°15′S
2. Counterclockwise rotations in the Late Eocene–Oligocene volcanic fields of San Luis Potosí and Sierra de Guanajuato (eastern Mesa Central, Mexico)
3. Space-geodetic estimation of the nazca-south america euler vector
4. Seismological aspects of the 1988–1989 Lonquimay (Chile) volcanic eruption
5. Paleomagnetism of the North Patagonian batholith, southern Chile. An exercise in shape analysis
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