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<p> Dear Colleagues, <br>
</p>
<p>the deadline for the abstract submission is on January 15th and
thus we would like to draw your attention and invite you to
consider submitting an abstract to the session <b class="">ST5.15
</b><b class="">Seismotectonics of the Marmara Sea</b> to be held
at the EGU General Assembly 2020, May 3–8, in Vienna. </p>
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<div class=""><b class="">Abstract submission: </b><a
class="moz-txt-link-freetext"
href="https://meetingorganizer.copernicus.org/EGU2020/session/37996"
moz-do-not-send="true">https://meetingorganizer.copernicus.org/EGU2020/session/37996</a></div>
<div class=""> <br>
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<div class=""><u><b class="">Session: ST5.15 Details<br>
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<u> </u>
<div class="col-md-5 "><u> </u>The continuation of the
North Anatolian fault below the Marmara Sea is the segment
where the next strong earthquake is expected after the
1999 Izmit event. Since the city of Istanbul is very close
to the seismic gap the seismic risk is probably very high.
Furthermore, the fault seems to be mature given the fact
that the last major event struck the area in 1766 and a
return period of approximately 250 years. However, to
assess the hazard and risk in detail a number of open
scientific key question have to be addressed that are
critical to assess the seismic hazard in terms of maximum
earthquake magnitude, location, nucleation area and
rupture propagation direction. To better address these
questions an integration of different geo-disciplines is
essential in order to better describe the structural
setting, rheology, temperature and density distribution,
spatio-temporal deformation and all kinds of observation
data ranging from satellite geodesy, seismology,
geological to geomorphological.</div>
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<div class="col-md-5 "> The main goal of this session is to
bring together researchers from various geodisciplines
that contribute to a thorough understanding of the driving
processes below the Sea of Marmara on different
spatio-temporal scales. Furthermore, it is intended to
identify open key-questions and future challenges.
Contributions may regard, but are not limited to, studies
of: <br>
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<div class="col-md-5 "><br>
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<div class="col-md-5 ">- Seismic Monitoring of the Marmara
seismic gap<br>
- Historical seismicity and paleoseismological
investigations<br>
- Co-, inter- and post-seismic observations and models<br>
- Forward and inverse models of THM-processes and 3D
subsurface structure<br>
- Structural investigations from active profiling,
receiver functions and tomography<br>
- Interpretation and modelling of stress and strain
observations<br>
- Finite geologic strain versus geodetic strain<br>
- Relationship between crustal deformation, heat flow and
seismicity<br>
- Seismic hazard and risk assessment and early warning
systems</div>
<p><span class="" style="font-style: normal;"><b class="">Confirmed
invited speaker</b> is <b>Pierre Henry</b> (CEREGE,
Aix Marseille Univ., CNRS, IRD, INRA, Coll. France,
Aix-Marseille, France) who will give an overview talk<i>.</i></span><span
class=""></span></p>
<div class="">We look forward to receiving your
contributions and thank you very much for your attention.</div>
<div class=""><br class="">
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<div class="">Sincerely yours, session conveners,<br>
Oliver Heidbach<br>
Marco Bohnhoff<br>
Murat Nurlu<br>
</div>
<div class="">Magdalena Scheck-Wenderoth</div>
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<pre class="moz-signature" cols="72"><font size="-1">------------------------------------------------------------
Dr. Oliver Heidbach
Head of the World Stress Map Project
Helmholtz Centre Potsdam
GFZ German Research Centre for Geosciences
Section 2.6 Seismic Hazard and Risk Dynamics
Telegrafenberg
14473 Potsdam
Germany
phone: +49(0)331 288-2814
fax: +49(0)331 288-1127
e-mail: <a class="moz-txt-link-abbreviated" href="mailto:heidbach@gfz-potsdam.de" moz-do-not-send="true">heidbach@gfz-potsdam.de</a>
web: <a class="moz-txt-link-freetext" href="http://www.gfz-potsdam.de" moz-do-not-send="true">http://www.gfz-potsdam.de</a>
<a class="moz-txt-link-freetext" href="http://www.world-stress-map.org" moz-do-not-send="true">http://www.world-stress-map.org</a>
------------------------------------------------------------</font></pre>
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