Brief cessations of geothermal production can induce seismicity, a phenomenon that has
drawn increasing attention in recent years. Such observations are rare, and the underlying …

We present an updated and validated seismic catalog for the northern Fennoscandian
region, focusing on postglacial faults from the Merasjärvi fault system in the southwest to the …

Seamounts and ridges are often invoked to explain subduction‐related phenomena such as
flat slab generation, but the extent of their involvement remains controversial. An analysis of …

Slow slip events (SSEs) are transient slip episodes taking place along the plate interface of
subduction zones. They usually occur synchronously to tectonic tremors and/or seismic …

Estimates of the onset times of P phases from active source experiments can effectively be
used in develo** wavespeed models, and the large number of recordings typical of such …

Les modes de glissement sur l'interface de subduction varient du glissement asismique
stable à la rupture sismique rapide en passant par des glissements transitoires lents dont la …

The Hikurangi subduction zone is located at the south end of the 300 km-long Tonga-
Kermadec-Hikurangi subduction system, where the Pacific plate subducts westward under …