The seismic and volcanological structure of Deception Island (Antarctica) is an intense focus
topic in Volcano Geophysics. The interpretations given by scientists on the origin, nature …

This paper shows a new multidisciplinary interpretation approach to the internal structure of
Tenerife Island. The central core of this work is the determination of the three-dimensional …

Passive high‐resolution attenuation tomography is used here to image the geological
structure in the first upper 4 km of the shallow crust beneath the Campi Flegrei caldera …

Mapping fluid accumulation in the crust is pertinent for numerous applications including
volcanic hazard assessment, geothermal energy generation, and mineral exploration. Here …

The complex volcanic system of Tenerife Island is known to have a highly heterogeneous
character, as recently confirmed by velocity tomography. We present new information …

Scattered seismic coda waves are frequently used to characterize small scale medium
heterogeneities, intrinsic attenuation or temporal changes of wave velocity. Spatial variability …

The Pollino range is a region of slow deformation where earthquakes generally nucleate on
low-angle normal faults. Recent studies have mapped fault structures and identified fluid …

Volcanoes produce a wide variety of seismic signals originating from a number of
mechanisms, ranging from the complex interaction between multiphase fluids and their …

The potential of the island of La Palma (Canary Islands) to host geothermal resources is very
high, mainly due to its high volcanic activity. The primary goal of this study is to get a …

In this paper we present innovative methodologies for seismic monitoring of volcanic
structures in space and time (4D) which can possibly evolve toward an unrest stage. They …