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Fracture and damage localization in volcanic edifice rocks from El Hierro, Stromboli and Tenerife
Authors
A Griffith
A Schubnel
+22 more
A Tibaldi
A Tibaldi
D Healy
DG Masson
J Martí
JW Neuberg
L Siena De
M Fazio
M Hürlimann
M Paulatto
MJ Heap
MJ Heap
MJR Gee
P Baud
P Benson
PD Harris
PM Benson
PR Sammonds
R Urgeles
S Falsaperla
S Vinciguerra
S Vinciguerra
Publication date
1 January 2018
Publisher
'Springer Science and Business Media LLC'
Doi
Cite
Abstract
© 2018 The Author(s). We present elastic wave velocity and strength data from a suite of three volcanic rocks taken from the volcanic edifices of El Hierro and Tenerife (Canary Islands, Spain), and Stromboli (Aeolian Islands, Italy). These rocks span a range of porosity and are taken from volcanoes that suffer from edifice instability. We measure elastic wave velocities at known incident angles to the generated through-going fault as a function of imposed strain, and examine the effect of the damage zone on P-wave velocity. Such data are important as field measurements of elastic wave tomography are key tools for understanding volcanic regions, yet hidden fractures are likely to have a significant effect on elastic wave velocity. We then use elastic wave velocity evolution to calculate concomitant crack density evolution which ranges from 0 to 0.17: highest values were correlated to the damage zone in rocks with the highest initial porosity
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