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Lower panel: Schematic models of Tenerife magmatic system and modified resistivity models used for the phonolitic magma chambers study.
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In order to analyse each case separately, we modified the resistivity model of Piña-Varas et al. (2015) by adding new structures taking into account the magma chambers proposed on these studies.
Resistivity models can be described as two layered.
3-D resistivity models used to perform the sensitivity tests.
Resistivity models near the spreading axis generally have a lower resistivity than those in the off-axis area.
The results are compared with bulk resistivity models.
To determine the appropriate range of resistivity in each zone, we constructed representative resistivity models in which the resistivity in each zone was replaced with a number of resistivity values.
(b) Appropriate range of resistivity within zone C2 We constructed representative resistivity models in which we replaced the resistivity in zone C2 with one of five resistivity values (20, 50, 100, 200, 300 Ω m).
Resistivity models were corroborated by simultaneous measurements of salinity in nearby piezometers.
Processed data and 1D resistivity models were provided by this project.
A fluid-bearing asymmetric damage zone representative of resistivity models is drawn around the Ganos Fault.
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