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Dear colleagues,

Since abstract submission deadline is approaching fast, we join the 
endless line of reminder emails and draw your attention back to the new 
PICO session '*Dynamics of dilatant faults and fractures (co-organized, 
TS2.4/GD2.13)*' at EGU 2019.
The session focuses on all aspects of dilatant and hybrid failure in 
rocks from micro- to macroscale, from fracturing to faulting (see 
session abstract below).

We invite contributions from numerical and analog modeling, field work, 
geophysics and other methods in the disciplines of geomechanics, fluid 
rock interactions, mineralogy, hydrology and age dating.
This session aims to bring together researchers with interest in 
dilatant faults and fractures, that have been scattered over multiple 
sessions in the past years.

Follow this link for more information and abstract submission: 
https://meetingorganizer.copernicus.org/EGU2019/session/30737

*
**Deadline for abstract submission: January 10th, 2019*


Looking forward to an exciting session at EGU,

Best Regards,

Michael Kettermann & Christoph von Hagke


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Session description: TS2.4/GD2.13

*Dynamics of dilatant faults and fractures (co-organized) PICO session*

Dilatant faults and fractures are ubiquitous crustal features that form 
major pathways for fluid flow, such as water, hydrocarbons, or magma, 
and consequently are of great interest for water and energy supply, 
geohazard assessment and geodynamics. However, little is known about 
their detailed structure at depth, their surface expression, and the 
transition of failure modes from dilatant to shear. Reasons for this 
lack of understanding is the enormous complexity of dilatant fractures 
due to the influence of parameters such as lithology, fault kinematics 
and mechanical stratigraphy. Therefore, the time and space evolution as 
well as the seismic hazard potential are largely unresolved.
In this session we invite contributions addressing all aspects of 
dilatant faulting and fracturing. We aim to stimulate discussion by 
integrating geophysical and outcrop studies as well as analog and 
numerical modeling. We particularly invite studies on all scales 
focusing on analyses of surface processes, topography, fault/fracture 
geometry, poro-perm characteristics, fluid flux modeling, age dating or 
kinematic reconstruction. We aim at providing a forum for all 
disciplines concerned with the dynamics of dilatant faulting and 
fracturing to meet and discuss their views.

-- 
__________________________________________________
Dr. Michael Kettermann
Structural Geology, Tectonics and Geomechanics
RWTH Aachen University
Lochnerstraße 4-20, 52056 Aachen, Germany
Room 314a
+49 (0)241 80-98439


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