<div dir="ltr"><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)">Dear colleagues, we are glad to invite you to take part in the special issue of the Journal of Earth Sciences of South America!!! Please, see below.</span><div><br></div><div><br></div><div>:::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::</div><div><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)">Journal South American Earth Sciences - ELSEVIER</span><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)">Special issue: Famatinian orogen on the South American plate</span><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)"> </span><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)">Edited by Pablo Alasino, César Casquet, Mariano Larrovere, Juan Dahlquist</span><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)">The Famatinian orogeny was an accretionary-type orogeny that took place in the Ordovician along the proto-Andean margin of Gondwana from Patagonia to Venezuela. It was part of the ca. 14,000 km Terra Australis orogeny that fringed the SW Gondwana margin and whose activity continues to date as the Andean orogeny. The exposure of Famatinian rocks along the edge of the South American plate is varied and the orogenic belt provides an ideal natural laboratory to explore the evolution of long lived magmatic systems and the reconstruction of tectonic and sedimentary records. Hence, the Journal of South American Earth Sciences openly calls for papers for a special issue on this subject.</span><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)">This special volume of the JSAES is aimed at publishing new contributions focused on physical and chemical processes involved the evolution of the Famatinian orogen - from the innermost to the atmosphere.</span><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)"> </span><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)">Researchers who may be interested in participating in this special issue are invited to send tentative titles.</span><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)">We will be happy to receive your proposals!!!</span><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)">Key dates:</span><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)">- Submission deadline of tentative titles is May 10th, 2019</span><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)"> </span><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)">- Submission deadline of manuscripts is March 20th, 2020</span><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)">- Second half of 2020 – Publication in Journal of South American Earth Sciences</span><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)">Best regards,</span><br style="font-size:13.3333px;color:rgb(51,51,51);font-family:monospace"><span style="color:rgb(51,51,51);font-family:monospace;font-size:13.3333px;background-color:rgb(253,253,253)">Pablo on behalf of the editorial board</span> <br clear="all"><div><br></div>-- <br><div dir="ltr" class="gmail_signature" data-smartmail="gmail_signature"><div dir="ltr">Pablo H. Alasino<br>INGeReN-UNLaR // CONICET<br>ARGENTINA</div></div></div></div><div id="DAB4FAD8-2DD7-40BB-A1B8-4E2AA1F9FDF2"><br> <table style="border-top:1px solid #d3d4de">
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