Investigating the Gravity Signatures of the Margin-Oblique Deep Seated Andean Faults in the Rio Teno Region of the Transitional Southern Volcanic Zone, Chile

Abstract

In a tectonic regime dominated by North-South oriented convergent stresses, margin oblique lineaments in the main cordillera of the Chilean Andes are theorized to significantly contribute to the dynamic evolution of this mountain belt as hydrothermal and