Midcrustal Deformation in the Central Andes Constrained by Radial Anisotropy

The Central Andes are characterized by one of the largest orogenic plateaus worldwide. As a result, they are home to some of the thickest continental crust observed today (up to ~75‐km thick). Understanding the response of the crust to such overthickening provides insights into the ductile behavior...

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Veröffentlicht in:	Journal of geophysical research. Solid earth 2018-06, Vol.123 (6), p.4798-4813
Hauptverfasser:	Lynner, Colton, Beck, Susan L., Zandt, George, Porritt, Robert W., Lin, Fan‐Chi, Eilon, Zachary C.
Format:	Artikel
Sprache:	eng
Schlagworte:	Ambient noise ambient noise tomography Anisotropy Central Andes Continental crust Crustal deformation crustal flow Crustal structure Deformation Deformation mechanisms Geophysics Heterogeneity Noise Orogeny Plateaus radial anisotropy Rayleigh waves Tomography Wave phase Wave velocity
Online-Zugang:	Volltext
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