[CIG-ALL] Reminder EGU 2018: "The Interplay between Earthquakes, the Seismic Cycle and Long-term Deformation: Models and Observations”

Luca Dal Zilio dalzilio.luca at gmail.com
Fri Jan 5 02:50:17 PST 2018


Dear colleagues,

A quick reminder for an exciting and multidisciplinary session at the next EGU General Assembly in Vienna (8-13 April 2018):

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The Interplay between Earthquakes, the Seismic Cycle and Long-term Deformation: Models and Observations

[TS5.2/G3.9/GD2.8/NH4.9/SM 2.07]

Invited speaker: Marion Thomas, Oxford University
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Join us at next EGU (Spring 2018) in Vienna and submit an abstract by clicking here:  http://meetingorganizer.copernicus.org/EGU2018/session/27072 <http://meetingorganizer.copernicus.org/EGU2018/session/27072>

Attention: The abstract submission deadline is Wednesday January 10, 2018 @ 13:00 CET.

With best regards,

Luca Dal Zilio (ETH Zürich)
Marcel Thielmann (Uni-Bayreuth)
Romain Jolivet (ENS Paris)
Jean-Philippe Avouac (Caltech)
Ylona van Dinther (ETH Zürich)

–––– Session description ––––

Long- and short-term tectonic processes shape the stress conditions under which faults operate. At the time scale of the earthquake cycle, these stresses are released by various modes of deformation ranging from steady, aseismic deformation to dynamic, seismic slip on faults. The physical processes in action at the various characteristic spatial and temporal scales motivate the integration of dynamic rupture and short term fault processes with long-term crustal deformation modeling. Reconciling observations and mechanisms will improve our understanding of the physical processes governing the seismic cycle and the construction of topography and geological  structures, the rheology of the lithosphere-asthenosphere system. 

Specific questions include: How long-term crustal and lithospheric dynamics and structures affect short-term seismicity and earthquake cycle behaviour? How earthquake cycles result in the construction of topographic features? What are the relative contributions of rheology (temperature, fluids, chemistry) and geometry behaviour of seismic and aseismic slip? What are the roles of faulting and off-fault deformation in shaping the landscape and partitioning seismic and aseismic energy dissipation? These example questions are intended to stimulate a discussion about the interplay between seismicity, earthquake cycle dynamics and the geological and geodynamic evolution of deforming zones. We seek contributions from across the fields of geology, geodynamics, seismology and geodesy, encouraging both modelling and observational studies.

For more information on the session, please visit: http://meetingorganizer.copernicus.org/EGU2018/session/27072 <http://meetingorganizer.copernicus.org/EGU2018/session/27072>
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