Evidence and models for lower crustal flow beneath the Galápagos platform

Author:

Orellana-Rovirosa Felipe1,Richards Mark1

Affiliation:

1. Department of Earth and Planetary Science; University of California; Berkeley California USA

Funder

the US National Science Foundation and CONICYT

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference42 articles.

1. Drowned islands downstream from the Galápagos hotspot imply extended speciation times;Christie;Nature,1992

2. Morphological and geochemical variations along the eastern Galápagos Spreading Center;Christie;Geochem. Geophys. Geosyst.,2005

3. Control of high oceanic features and subduction channel on earthquake ruptures along the Chile-Peru subduction zone;Contreras-Reyes;Phys. Earth Planet. Int.,2011

4. Global kinematics in deep versus shallow hotspot reference frames;Cuffaro;Geol. Soc. Am. Spec. Pap.,2007

5. Morphology and dynamics of inflated subaqueous basaltic lava flows;Deschamps;Geochem. Geophys. Geosyst.,2014

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