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<p class="x_x_x_MsoNormal"><span class="">Dear all,</span></p>
<p class="x_x_x_MsoNormal"><span class=""><b class="">Aubreya Adams</b> is “Geophysics” faculty candidate. </span>The talk is scheduled at
<b class="">3</b><b class="">:30 PM </b>on<b class=""> 24<sup class="">th</sup> February 2021</b> (Wednesday). </p>
<p class="x_x_x_MsoNormal">Zoom: <a target="_blank" href="https://fsu.zoom.us/j/99359267833" class="" style="box-sizing:border-box; background-color:rgb(255,255,255); color:rgb(14,113,235); text-decoration:none; font-variant-ligatures:normal; orphans:2; widows:2">https://fsu.zoom.us/j/99359267833</a></p>
<div class="">Please email me: <a href="mailto:mmmookherjee@fsu.edu" class="">mmookherjee@fsu.edu</a> and let me know if you would like to meet the candidate.</div>
<p class="x_x_x_MsoNormal"><b class="">Title</b>: Heterogeneity in the Alaskan Subduction Zone</p>
<p class="x_x_MsoNormal"><b class="">Abstract</b>: The Alaskan Subduction Zone is home to numerous earthquakes and volcanic eruptions – yet these geological hazards are not evenly distributed along the boundary. Zones that have generated megathrust earthquakes
like the 1964 Good Friday Earthquake, the second largest earthquake in recorded history, border zones that have not generated large earthquakes in thousands of years. To investigate the root causes of these observed variabilities, an amphibious array of 105
broadband seismometers spanning the southern Alaskan coast collected 15 months of continuous ground motion data. These data are now being used to image the deep lithosphere and asthenosphere along the subduction zone using surface wave tomography. Models
built from this technique will illuminate how differences in deep processes and structures may influence surficial tectonic behaviors and hazards.</p>
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<div class="">Thank you</div>
<div class="">Mainak</div>
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