Publication Date:
2021-01-27
Description:
The brittle-ductile transition (BDT) separates the lower crust where deformation occurs in steady-state regime, from the upper crust where it is rather dominated by stick-slip.
The fault hangingwall above BDT accumulates elastic energy during the interseismic period, without significant evidence of surface strain rate
Faults activate in areas of high strain rate gradients along the segments with lower strain rates
Fluid discharge varies as a function of the tectonic setting
The phenomenology gives insights for the parameters to be monitored in earthquake forecasting
Description:
Italian Presidenza del Consiglio dei Ministri - Dipartimento della Protezione Civile (DPC) within the INGV-DPC 2007-2009 agreement(project S1), Sapienza University and CNR-Eurocores-TopoEurope.
Description:
Unpublished
Description:
Brisbane Australia
Description:
3.2. Tettonica attiva
Description:
open
Keywords:
brittle-ductile transition
;
L' Aquila 2009 earthquake
;
Emilia 2012 earthquake
;
geodetic strain rate
;
fault activation
;
magnitude
;
04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations
;
04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology
Repository Name:
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
Type:
Poster session
Permalink