Tracing Geophysical Indicators of Fluid‐Induced Serpentinization in the Pampean Flat Slab of Central Chile
Open Access
- 9 September 2019
- journal article
- research article
- Published by American Geophysical Union (AGU) in Geochemistry, Geophysics, Geosystems
- Vol. 20 (9), 4408-4425
- https://doi.org/10.1029/2019gc008491
Abstract
No abstract availableKeywords
Funding Information
- National Science Foundation (EAR‐1764271)
This publication has 78 references indexed in Scilit:
- Pressure–temperature estimates of the lizardite/antigorite transition in high pressure serpentinitesLithos, 2013
- Receiver function study of the Cascadia megathrust: Evidence for localized serpentinizationGeochemistry, Geophysics, Geosystems, 2009
- Mantle wedge anisotropy in Southern Tyrrhenian Subduction Zone (Italy), from receiver function analysisTectonophysics, 2008
- Anisotropy and mantle flow in the Chile‐Argentina subduction zone from shear wave splitting analysisGeophysical Research Letters, 2004
- Seismic investigations of the O'Higgins Seamount Group and Juan Fernández Ridge: Aseismic ridge emplacement and lithosphere hydrationTectonics, 2004
- The importance of serpentinite mylonites for subduction and exhumation of oceanic crustTectonophysics, 2000
- Seismological evidence for the existence of serpentinized wedge mantleGeophysical Research Letters, 2000
- Relationship between anisotropy of P and S wave velocities and anisotropy of attenuation in serpentinite and amphiboliteJournal of Geophysical Research, 1997
- Magmatic evidence for Neogene lithospheric evolution of the central Andean “flat-slab” between 30°S and 32°STectonophysics, 1996
- Cenozoic tectonics of the High Andes of west-central Argentina (30–36°S latitude)Tectonophysics, 1996