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Call for application of 11 PhD positions in the Marie Sklodowska-Curie Doctoral Network “TREAD: daTa and pRocesses in sEismic hAzarD” project

We are seeking motivated young MSc students for a PhD position available at CEREGE within the Marie Sklodowska-Curie Doctoral Network “TREAD: daTa and pRocessess in sEismic hAzarD” on « Linking fault damage zone mechanical and geometrical characteristics with fault seismic history ».

 
Objectives: The objective of this PhD is to study the links between coseismic slip distribution, fault segmentation and associated damage zones. Indeed recent studies suggest that such large variations in slip are possibly due to the presence of barrier zones that stop the rupture. The knowledge accumulated at University of Padova (Italy) on damage zones distribution and their mechanical properties on one hand, and the experience in mapping active faults and acquiring their seismic history gained by CEREGE over the last 10 years, will allow the PhD student to study those links. In particular, the surface expression of the fault based on the quantification of cumulative displacement (e.g. faceted spurs, fault scarps, geological displacement) along with the accurate mapping of the active portions of the fault will allow him/her to relate slip distribution with fault segmentation, damage and their link with inherited structures. Several sites will be selected on faults displaying different damage zone characteristics and fault cumulative displacement (e.g. the Vado di Corno fault, the Roccapreturo fault) in the Apennines, to quantify geometrical characteristics such as fault length, specific geometrical features in the fault surface expression such as bends, steps of a few km, maximum cumulative displacement, thickness of damage zone, degree of fracturation, specific mechanical properties, using high resolution topography based on digital elevation model acquired from Lidar drone or photogrammetry. Moreover, the fault slip-rate and, if the sites are suitable, its seismic history, will be estimated with 36Cl fault scarp dating and dating of offset markers. Those data will allow the PhD student to unravel how fault maturity, coseismic rupture extent and clustering (coefficient of variation between slip rate and earthquake occurrence) are linked. 
PhD should start between September and November 2023.
 
See the details to apply on this link. 
Deadline for applications: April 30, 2023
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