Shallow Anatomy of the San Ramón Fault (Chile) Constrained by Geophysical Methods: Implications for its Role in the Andean Deformation

Author:

Yáñez G.12ORCID,Perez‐Estay N.34,Araya‐Vargas J.13ORCID,Sanhueza J.12ORCID,Figueroa R.135,Maringue J.1,Rojas T.6

Affiliation:

1. Departamento de Ingeniería Estructural y Geotécnica Pontificia Universidad Católica de Chile Santiago Chile

2. Millenium Nucleus for Metal Tracing Along Subduction Universidad de Chile Santiago Chile

3. Centro de Excelencia en Geotermia de los Andes (CEGA) Universidad de Chile Santiago Chile

4. Dirección nacional de fronteras y límites del Estado (Difrol) Ministerio de relaciones exteriores Santiago Chile

5. Aluvial Consultores SPA., Providencia Santiago Chile

6. TRV Geofísica SPA Santiago Chile

Funder

Fondo Nacional de Desarrollo Científico, Tecnológico y de Innovación Tecnológica

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference70 articles.

1. Foreland shortening and crustal balancing in the Andes at 30°S latitude

2. Equations for the Estimation of Strong Ground Motions from Shallow Crustal Earthquakes Using Data from Europe and the Middle East: Vertical Peak Ground Acceleration and Spectral Acceleration

3. The crustal seismicity of the western Andean thrust (central Chile, 33–34°S): Implications for regional tectonics and seismic hazard in the Santiago area;Ammirati J. B.;Bulletin of the Seismological Society of America,2019

4. Space-geodetic estimation of the nazca-south america euler vector

5. The west Andean thrust, the San Ramón fault, and the seismic hazard for Santiago, Chile;Armijo R.;Tectonics,2010

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