4D imaging of the seismic energy release before the 2011 El Hierro eruption (Canary Islands)

Author(s):  
Rubén García-Hernández ◽  
Luca D'Auria ◽  
José Barrancos ◽  
Germán D. Padilla

<p>The estimation of the spatial and temporal variations of the b-value of the Gutenberg-Richter law is of great importance in different seismological applications. However, its estimate is strongly dependent upon the selected spatial and/or temporal scale due to the heterogeneous distribution of the seismicity. This is especially relevant in volcanic and geothermal areas where dense clusters of earthquakes often overlap to the background seismicity.</p><p>For this reason, we propose a novel multiscale approach allowing a consistent estimation of the b-value regardless of the considered spatial and/or temporal scales. Our method, named <strong>MUST-B</strong> (<strong>MU</strong>ltiscale <strong>S</strong>patial and <strong>T</strong>emporal estimation of the <strong>B</strong>-value), basically consists in computing estimates of the b-value at multiple temporal and spatial scales, extracting for a given spatio-temporal point a statistical estimator of its value, as well as an indication of the characteristic spatio-temporal scale. This approach includes also a consistent estimation of the completeness magnitude (M<sub>c</sub>) and of the uncertainties over both b and M<sub>c</sub>, as well as, estimates of the seismic energy release rates.</p><p>We applied this method to the seismic datasets of El Hierro submarine eruption, started on October 2011 and linked to a precursor seismic unrest episode that initiated on July 2011. The seismicity showed a very complex spatial distribution, which also changed over time, showing a migration from the north of the island to the south. Results show that the high resolution 4D mapping is of great importance to understand the distribution of the seismic energy release in volcanic islands, which is possibly correlated to a variable geothermal fluid flow paths and/or magmatic sources. What is also remarkable is that even in highly heterogeneous catalogues, as for the 2011 El Hierro dataset, the MUST-B method could provide reliable estimates.</p>

1975 ◽  
Vol 65 (2) ◽  
pp. 351-357
Author(s):  
John Filson ◽  
Tom Simkin

abstract The Kolomogorov model of event occurrence as developed by Knopoff in earthquake model studies has been applied to a volcanic earthquake swarm. It is shown that in this case, where the rate of seismic energy release was nearly constant in time, the model adequately relates the various seismicity statistics of the swarm.


1993 ◽  
Vol 60 (2) ◽  
pp. 93-108 ◽  
Author(s):  
Ioannis Liritzis ◽  
Theodoros M. Tsapanos

1981 ◽  
Vol 86 (B1) ◽  
pp. 378 ◽  
Author(s):  
Neal R. Goins ◽  
Anton M. Dainty ◽  
M. Nafi Toksöz

Author(s):  
P. G. Dyadkov ◽  
Y. M. Romanenko ◽  
M. P. Kozlova ◽  
L. V. Tsibizov ◽  
A. A. Duchkova

Based on the joint analysis of the seismic regime parameters, such as anomalies of seismic energy release, b-value, seismic activity A10, approaches to assess the state of the block-seismic medium are proposed. The method validation was done for the example of preparation and development of seismic activity in 2008-2011 in the Central part of the Baikal rift, during which there were 2 strong M5.3 earthquakes. It was found that within 2 years before the strong Maximihinskoye Earthquake of 2008 in the Earth's crust of the epicentral region there is a transformation from softening to strengthening (consolidation) of the block medium. At the same time, in the neighboring region (the area of the Svyatoy Nos Peninsula), the opposite nature of the changes is observed.


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