The thermal structure of subduction zones is fundamental to our understanding of physical
and chemical processes that occur at active convergent plate margins. These include …

In this review article, we compile seismological observations from the different constituent
parts of the Northern Chile forearc: the downgoing Nazca Plate, the plate interface, the …

We search for earthquake swarms along the Chilean subduction, from− 18° to− 39° of
latitude, 2003–2020 by develo** an objective, model-based method that detects potential …

Metamorphic olivine formed by the reaction of antigorite+ brucite is widespread in
serpentinites that crop out in glacier-polished outcrops at the Unterer Theodulglacier …

Double seismic zones (DSZs), parallel planes of intermediate‐depth earthquakes inside
oceanic slabs, have been observed in a number of subduction zones and may be a …

Recordings of earthquakes by a temporary deployment of 84 short period seismometers in
northern Chile were used to derive regional 3D seismic velocity models for the Taltal …

We compute stress drops for earthquakes in Northern Chile recorded between 2007 and
2021. By applying two analysis techniques,(a) the spectral ratio (SR) method and (b) the …

We investigate the variations of the seismic source properties and aftershock activity using
kinematic inversions and template-matching for six large magnitude intermediate-depth …

We used data from> 100 permanent and temporary seismic stations to investigate seismicity
patterns related to the 1 April 2014 M8. 1 Iquique earthquake in northern Chile. Applying a …

Stress drop is an earthquake property indicative for the characteristic relation of slip to fault
dimension. It is furthermore affected by fault strength, fault topography, the presence of …