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Diana Comte
University of ChileMeeting roles in:
High-Frequency Seismic Imaging of the Crust Beneath the Puna Plateau of the Central Andes using Local Earthquake Autocorrelation
Orogen-wide Crustal Architecture Across the Southern Volcanic Zone (~36⁰S) in the Andes of South America Revealed by Teleseismic Receiver Functions
Detachment Involved Deformation in the Santa Barbara System in NW Argentina Revealed by Seismicity and Receiver Functions
Variable Slab Geometry and Mantle Wedge Structure Along the Central and Southern Andean Subduction Zone from Finite-Frequency Teleseismic Tomography
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