The Chilean subduction zone hosts M w> 8 earthquakes, which could trigger earthquakes
on crustal faults located along the plate margin. Using synthetic earthquakes from a quasi …

The Alhué mining district (AMD) of the Coastal Range in Central Chile is situated
approximately 70 km southwest of the city of Santiago and hosted in stratified Jurassic and …

Landslides in deglaciated and deglaciating mountains represent a major hazard, but their
distribution at the spatial scale of entire mountain belts has rarely been studied. Traditional …

Abstract In the South‐Central Andes, the crustal structures driving the tectonic evolution of
the Andean Cordillera remain unresolved. So far, most seismological studies focused on the …

The compilation of a database of 225 strain/stress tensors (accounting for~ 4000 fault-striae
data pairs) combined with evidence of syntectonic strata, and a seismotectonic appraisal …

The Patagonian slab window (PSW) is a region of the Southamerican subduction zone
where the absence of subducted slabs is interpreted, due to the subduction of the Chile Mid …

Grabens, or valleys formed during extensional tectonic events, are common but rarely
observed during formation. In November 2023, inelastic surface deformation formed abruptly …

Structural inheritance is a major control on the Andean structural architecture and magma
emplacement, particularly in Patagonia, where the genesis of sedimentary basins and …

Replying to: R. Vassallo et al.; Scientific Reports https://doi. org/10.1038/s41598-024-66469-
0 (2024). In this paper we address interest on our recent research 1 brought up by Vassallo …

Determining the eruption frequency-Magnitude (fM) relationship for data-limited volcanoes is
challenging since it requires a comprehensive eruption record of the past eruptive activity …