The models presented below explain several features of the preparatory processes leading to the M = 6.6 earthquake of June 17th 2000 in the SISZ (Stefansson et al., 2011). Strong similarities between the SISZ and the TFZ encourage to apply a similar conceptual model to describe the preparatory processes expected to take place before the next large earthquake in North Iceland.
M. Bonafede, R. Stefansson (2014). Heterogeneities, asperities, fluid migration and seismicity. Húsavík -IS : Husavik Academic Center.
Heterogeneities, asperities, fluid migration and seismicity
BONAFEDE, MAURIZIO;
2014
Abstract
The models presented below explain several features of the preparatory processes leading to the M = 6.6 earthquake of June 17th 2000 in the SISZ (Stefansson et al., 2011). Strong similarities between the SISZ and the TFZ encourage to apply a similar conceptual model to describe the preparatory processes expected to take place before the next large earthquake in North Iceland.File in questo prodotto:
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