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  5. A forward test for interaction between remote earthquakes and volcanic eruptions: the case of Sumatra (June 2000) and Denali (November 2002) earthquakes
 
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A forward test for interaction between remote earthquakes and volcanic eruptions: the case of Sumatra (June 2000) and Denali (November 2002) earthquakes

Author(s)
Selva, J.
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia  
Marzocchi, W.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia  
Zencher, F.  
Alma Mater Studiorum, Universita` di Bologna  
Casarotti, E.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Piersanti, A.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Boschi, E.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione AC, Roma, Italia  
Language
English
Obiettivo Specifico
3.6. Fisica del vulcanismo
Status
Published
JCR Journal
JCR Journal
Journal
Earth and planetary science letters  
Issue/vol(year)
/226(2004)
ISSN
0012-821X
Electronic ISSN
1385-013X
Publisher
Elsevier Science Limited
Pages (printed)
383 – 395
Date Issued
September 2004
DOI
10.1016/j.epsl.2004.08.006
URI
https://www.earth-prints.org/handle/2122/8167
Subjects
04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous  
Subjects

earthquake–volcano in...

post-seismic stress p...

forward test

Engano earthquake

Denali earthquake

Abstract
We propose a formal procedure to validate the hypothesis of a causal relationship between great tectonic earthquakes and
volcanic eruptions through a forward statistical test. This approach allows such a hypothesis to be evaluated in an objective way,
ruling out any possible unconscious overfitting of the past data. The procedure consists of two steps: (a) the computation of the
stress perturbation in a volcanic area due to some selected seismic event, by means of a spherical, layered, viscoelastic and self-
gravitating earth model; and (b) the application of a statistical test to check the differences in the spatio-temporal distribution of
eruptions before and after the earthquake, weighting each eruption with the stress perturbation induced at the volcano at the time
of the eruption. Finally, for the sake of example, we apply the method to the case of the recent Engano earthquake in Sumatra
(June 2000) and the Denali earthquake in Alaska (November 2002).
Type
article
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Selva&al.,2004.pdf

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