<html><head>
<meta http-equiv="Content-Type" content="text/html; charset=utf-8">
</head>
<body style="word-wrap:break-word" vlink="#954F72" link="#0563C1" lang="EN-US">
<br>
<div class="moz-forward-container"><br>
<meta name="Generator" content="Microsoft Word 15 (filtered
medium)">
<style>@font-face
{font-family:"Cambria Math";
panose-1:2 4 5 3 5 4 6 3 2 4;}@font-face
{font-family:Calibri;
panose-1:2 15 5 2 2 2 4 3 2 4;}p.MsoNormal, li.MsoNormal, div.MsoNormal
{margin:0in;
font-size:11.0pt;
font-family:"Calibri",sans-serif;}a:link, span.MsoHyperlink
{mso-style-priority:99;
color:#0563C1;
text-decoration:underline;}span.EmailStyle17
{mso-style-type:personal-compose;
font-family:"Calibri",sans-serif;
color:windowtext;}.MsoChpDefault
{mso-style-type:export-only;
font-family:"Calibri",sans-serif;}div.WordSection1
{page:WordSection1;}</style><!--[if gte mso 9]><xml>
<o:shapedefaults v:ext="edit" spidmax="1026" />
</xml><![endif]--><!--[if gte mso 9]><xml>
<o:shapelayout v:ext="edit">
<o:idmap v:ext="edit" data="1" />
</o:shapelayout></xml><![endif]-->
<div class="WordSection1">
<p class="MsoNormal">Hi all,<o:p></o:p></p>
<p class="MsoNormal">This is a reminder of the EOAS colloquium
Today at 3 PM. The colloquium is in-person. I am sure his
research and background will be of interest to many different
groups and individuals.
<o:p></o:p></p>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal"><b>Everyone is invited to a FLUIDS
gathering (food and drinks) from Geology Club that will
immediately follow the colloquium.<o:p></o:p></b></p>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal">If you would like to meet with the speaker,
please email Jeremy Owens (<a href="mailto:jdowens@fsu.edu" moz-do-not-send="true" class="moz-txt-link-freetext">jdowens@fsu.edu</a>).
It would be great for him to meet with faculty and/or students
across the broad range of topics in our department.<o:p></o:p></p>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal"><u>Time</u>: 3 pm Friday, September 16<sup>th</sup>
<o:p></o:p></p>
<p class="MsoNormal"><u>Location</u>: 1050 EOA<o:p></o:p></p>
<p class="MsoNormal"><u>Speaker</u>: Dr. Besim Dragovic from the
University of South Carolina<o:p></o:p></p>
<p class="MsoNormal"><u><o:p><span style="text-decoration:none"> </span></o:p></u></p>
<p class="MsoNormal"><u>Title</u>: Constraining the rates of
subduction metamorphism and metasomatism using chronology and
chronometry: insights from the Eocene<o:p></o:p></p>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal"><u>Abstract</u>: <span style="font-family:"Times New Roman",serif">
High-pressure metamorphic rocks exhumed from subduction
zones offer the only direct samples of the subduction
interface, providing important information for understanding
active subduction zones. While the timing of subduction zone
metamorphism in exhumed terranes has been achievable using
geochronology, the timescales and rates of subduction zone
processes have been more elusive. However, approaches
utilizing multiple mineral-isotope systems, in-situ
techniques and/or microsampling of crystal growth domains
have provided important constraints on these processes. This
talk highlights the use of direct chronology and chronometry
from the subduction zone rock record, with particular
attention to examples from the Western Alps (Italy and
Switzerland).</span><o:p></o:p></p>
</div>
</div>
<pre class="moz-signature" cols="72">
</pre>
</body>
</html>