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<font face="Arial" size="2" class="">Dear colleagues, </font>
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<div class=""><font face="Arial" size="2" class="">**Sorry for the multiple cross-postings**<br class="">
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Please note that the #vEGU21 abstract submission deadline has been extended by one week to Wednesday
<b class="">20 January at 13:00 CET</b>! </font></div>
<div class=""><font face="Arial" size="2" class="">We would like to draw your attention, and hope that you will consider submitting an abstract, to the following multidisciplinary session: </font></div>
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<div class=""><b class=""><font face="Arial" class="" size="2">From Minerals to the Dynamics of Earth’s Interior:</font></b></div>
<div class=""><b class=""><font face="Arial" class="" size="2">linking crystal chemistry, rheology, and geodynamics across the scales </font></b></div>
<div class=""><font face="Arial" class="" size="2"><a href="https://protect-au.mimecast.com/s/nik2CmO5glurqWVpCGpZsr?domain=meetingorganizer.copernicus.org" class="">https://meetingorganizer.copernicus.org/EGU21/session/39795 </a></font></div>
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<div class=""><span class=""><font face="Arial" class="" size="2">We look forward to to meeting you online!</font></span></div>
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<div class=""><span class=""><font face="Arial" class="" size="2">Sincerely, </font></span></div>
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<div class=""><span class=""><font face="Arial" class="" size="2">Anna Gülcher (ETH Zürich, Switzerland)</font></span></div>
<div class=""><span class=""><font face="Arial" class="" size="2">Sebastian Ritterbex (Ehime University, Japan)</font></span></div>
<div class=""><span class=""><font face="Arial" class="" size="2">Jac van Driel (UCL, United Kingdom)</font></span></div>
<div class=""><span class=""><font face="Arial" class="" size="2">John Hernlund (ELSI, Tokyo Inst. of Technology, Japan)</font></span></div>
<div class=""><span class=""><font face="Arial" class="" size="2">Patrick Cordier (Université de Lille, France)</font></span></div>
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<div class=""><span class=""><font face="Arial" class="" size="2">—————————</font></span><span style="font-family: Arial; font-size: small;" class="">——————————</span><span style="font-family: Arial; font-size: small;" class="">————————— </span></div>
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<div class=""><font face="Arial" class="" size="2"><b class="">The dynamics and evolution of the Earth’s interior controlled by a spectrum of processes covering a wide range of length- and timescales. Key planetary phenomena such as plate tectonics and mantle
convection are in fact a symphony of interconnected multi-scale mechanisms. Coupling of rock deformation mechanisms across the scales, however, remains one of the fundamental challenges in terrestrial planet sciences.</b></font></div>
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<div class=""><font face="Arial" class="" size="2"><b class=""><span class="" style="background-color: white;">In this session, we </span><span lang="EN-US" class="" style="background-color: white;">aim to bring together researchers across different disciplines.
We </span><span class="" style="background-color: white;">invite contributions </span><span lang="EN-US" class="" style="background-color: white;">from </span><span class="" style="background-color: white;">observations, experiments, and modelling. Topics
may include, but are not restricted to, atomistic simulations, solid-state defo<font class="">rmation experiments, (micro-)structural analysis of minerals and rocks, dynamic modelling of Earth’s interior, and interactions between these scales. </font></span><span class=""><span class="" style="background-color: white;"><span class="">Ultimately,
we aim to create new paths for future research concerning multi-scale dynamics of planetary interiors.</span></span></span></b></font></div>
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