Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5781715 | Tectonophysics | 2017 | 52 Pages |
Abstract
Our work suggests that rheology and therefore the position of the brittle ductile transition exerts a role at regional scale for the occurrence of crustal seismicity, however crustal structures and lithology play the major role at a more local scale and therefore they need to be considered for a better understanding of earthquake distribution within the seismogenic layer.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
L. Chiaraluce, M.R. Barchi, S. Carannante, C. Collettini, F. Mirabella, C. Pauselli, L. Valoroso,