From quiescence to unrest: 20 years of satellite geodetic measurements at Santorini volcano, Greece
Periods of unrest at caldera‐forming volcanic systems characterized by increased rates of
seismicity and deformation are well documented. Some can be linked to eventual eruptive …
seismicity and deformation are well documented. Some can be linked to eventual eruptive …
Forecasting magma-chamber rupture at Santorini volcano, Greece
How much magma needs to be added to a shallow magma chamber to cause rupture, dyke
injection and a potential eruption? Models that yield reliable answers to this question are …
injection and a potential eruption? Models that yield reliable answers to this question are …
Present‐day crustal stress field in Greece inferred from regional‐scale damped inversion of earthquake focal mechanisms
KI Konstantinou, V Mouslopoulou… - Journal of …, 2017 - Wiley Online Library
In this study we utilize regional and teleseismic earthquake moment tensor solutions in order
to infer the contemporary crustal stress in the Greek region. We focus on crustal earthquakes …
to infer the contemporary crustal stress in the Greek region. We focus on crustal earthquakes …
Seismic imaging of Santorini: Subsurface constraints on caldera collapse and present-day magma recharge
Volcanic calderas are surface depressions formed by roof collapse following evacuation of
magma from an underlying reservoir. The mechanisms of caldera formation are debated and …
magma from an underlying reservoir. The mechanisms of caldera formation are debated and …
Tectonism and Its Relation to Magmatism Around Santorini Volcano From Upper Crustal P Wave Velocity
At extensional volcanic arcs, faulting often acts to localize magmatism. Santorini is located
on the extended continental crust of the Aegean microplate and is one of the most active …
on the extended continental crust of the Aegean microplate and is one of the most active …
A detailed seismic anisotropy study during the 2011–2012 unrest period in the Santorini Volcanic Complex
G Kaviris, P Papadimitriou, P Kravvariti… - Physics of the Earth and …, 2015 - Elsevier
Abstract The Santorini Volcanic Complex (SVC) is an area in the Southern Aegean (Greece)
which has been characterized by low seismicity rates for the last decades, especially in the …
which has been characterized by low seismicity rates for the last decades, especially in the …
Relationship between active faulting/fracturing and magmatism around Santorini: Seismic anisotropy from an active source tomography experiment
In extending volcanic arcs such as the Aegean, tectonic processes exert a significant control
on magmatism. Spanning scales from 1 to 10s of km, volcanic vents, edifices, and eruptive …
on magmatism. Spanning scales from 1 to 10s of km, volcanic vents, edifices, and eruptive …
Detailed velocity ratio mapping during the aftershock sequence as a tool to monitor the fluid activity within the fault plane
The rheological properties of Earth materials are expressed by their seismic velocities and
VP/VS ratio, which is easily obtained by the Wadati method. Its double-difference version …
VP/VS ratio, which is easily obtained by the Wadati method. Its double-difference version …
Time varying crustal anisotropy at Whakaari/White Island volcano
Abstract Whakaari/White Island has been the most active New Zealand volcano in the 21st
century, producing small phreatic and phreatomagmatic eruptions, which are hard to predict …
century, producing small phreatic and phreatomagmatic eruptions, which are hard to predict …
Time‐space modeling of the dynamics of Santorini volcano (Greece) during the 2011–2012 unrest
Abstract The 2011–2012 unrest of Santorini (Thera) volcano (Aegean Sea, Greece) was
associated with microseismicity confined to the Kameni Line (KL), a major tectonovolcanic …
associated with microseismicity confined to the Kameni Line (KL), a major tectonovolcanic …