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<p>Dear colleagues: this is to inform you the new dates for
submission of your contribution to the thematic issue "<b>New
advances in Paleomagnetic and Magnetic Fabric Studies in Latin
America" to be pulished in </b><b>The Journal of South American
Earth Sciences. </b>Up to date, we have received the commitment
for fifteen contributions that are listed below. If your
contribution is not in the list or if you have decided to submit a
new one, please send an email to <b><a
class="moz-txt-link-abbreviated"
href="mailto:augrap@yahoo.com.ar">augrap@yahoo.com.ar</a></b>,
indicating title and authors before the end of Februrary. You will
be able to upload your contribution from March 1st 2020. <b>Deadline
for submitting the manuscripts has been set as April 15th 2020</b>.
Invited Editors for this special issue are: Augusto Rapalini
(Argentina), Fernando Poblete (Chile), Cecilia Caballero (Mexico)
and Irene Raposo (Brasil). <br>
</p>
<p>Estimados colegas: este mensaje es para informarlos de las nuevas
fechas para el envío de sus contribuciones al número temático <b>"New
advances in Paleomagnetic and Magnetic Fabric Studies in Latin
America" que se publicará en </b><b>The Journal of South
American Earth Sciences</b>. A la fecha, hemos recibido el
compromiso de quince contribuciones que se listan más abajo. Si su
contribución no figura en la lista o se ha decidido por enviar una
nueva, por favor envie un email a <b><a
class="moz-txt-link-abbreviated"
href="mailto:latinmag2019@uoh.cl">augrap@yahoo.com.ar</a></b>,
indicando título y autores antes de fin de febrero. Podrán
comenzar a subir vuestras contribuciones a partir del 1 de marzo
de 2020. <b>Se ha fijado la nueva fecha límite para envío de los
manuscritos el 15 de abril de 2020</b>. Los editores de este
número especial somos: Augusto Rapalini (Argentina), Fernando
Poblete (Chile), Cecilia Caballero (México) e Irene Raposo
(Brasil) <br>
</p>
Prezados colegas: <span style="color: rgb(34, 34, 34); font-family: arial, sans-serif; font-size: 28px; font-style: normal; font-variant-ligatures: normal; font-variant-caps: normal; font-weight: 400; letter-spacing: normal; orphans: 2; text-align: left; text-indent: 0px; text-transform: none; white-space: pre-wrap; widows: 2; word-spacing: 0px; -webkit-text-stroke-width: 0px; background-color: rgb(248, 249, 250); text-decoration-style: initial; text-decoration-color: initial; display: inline !important; float: none;"><font size="-1">esta mensagem é para informar sobre as novas datas para o envio de suas contribuições ao número temático "</font></span><span style="color: rgb(34, 34, 34); font-family: arial, sans-serif; font-size: 28px; font-style: normal; font-variant-ligatures: normal; font-variant-caps: normal; font-weight: 400; letter-spacing: normal; orphans: 2; text-align: left; text-indent: 0px; text-transform: none; white-space: pre-wrap; widows: 2; word-spacing: 0px; -webkit-text-stroke-width: 0px; background-color: rgb(248, 249, 250); text-decoration-style: initial; text-decoration-color: initial; display: inline !important; float: none;"><font size="-1"><b>New advances in Paleomagnetic and Magnetic Fabric Studies in Latin America"</b>, <b>a ser publicado no The Journal of South American Earth Sciences</b>. Até o momento, recebemos o compromisso de quinze contribuições listadas abaixo. Se sua contribuição não estiver listada ou você decidiu enviar uma nova, envie um email para <font color="#0000ff"><a class="moz-txt-link-abbreviated" href="mailto:augrap@yahoo.com.ar">augrap@yahoo.com.ar</a></font>, indicando o título e os autores antes do final de fevereiro. Eles poderão começar a enviar suas contribuições a partir de 1º de março de 2020. <b>O novo prazo para envio de manuscritos foi estabelecido em 15 de abril de 2020</b></font>.</span>
<span tabindex="0" lang="pt"></span><span tabindex="0" lang="pt"> </span>Os
editores desta edição especial são: Augusto Rapalini (Argentina),
Fernando Poblete (Chile), Cecilia Caballero (México) e Irene Raposo
(Brasil).
<p>List of contributions</p>
<p> </p>
<p class="yiv9431367660ydp3fd7ada8msonormal"
style="margin-bottom:6.0pt; background:white"><span
style="font-family:"New serif",serif;
color:#1D2228;mso-ansi-language:EN-US" lang="EN-US">1)</span><span
style="font-family:"New serif",serif;
color:#1D2228;mso-ansi-language:EN-US" lang="EN-US"> </span><span
style="font-size:7.0pt;font-family:"New
serif",serif;color:#1D2228;mso-ansi-language: EN-US"
lang="EN-US"> </span><span style="font-family: "New
serif",serif;color:#1D2228;background:white;mso-ansi-language:EN-US"
lang="EN-US"> ANISOTROPY OF MAGNETIC SUSCEPTIBILITY AND
KINEMATIC ANALYSIS IN DEFORMED NEOGENE SEQUENCES, NW SIERRAS
PAMPEANAS (27°30´S): PRELIMINARY RESULTS. </span><span
style="font-family:"New
serif",serif;color:#1D2228;background:white;
mso-ansi-language:ES" lang="ES">Quiroga et al. </span><span
style="font-size:10.0pt;
font-family:"Helvetica",sans-serif;color:#1D2228"></span></p>
<p class="yiv9431367660ydp3fd7ada8msonormal"
style="margin-bottom:6.0pt; background:white"><span
style="font-family:"New serif",serif;
color:#1D2228;mso-ansi-language:EN-US" lang="EN-US">2)</span><span
style="font-size:7.0pt;font-family:"New
serif",serif;color:#1D2228;mso-ansi-language: EN-US"
lang="EN-US"> </span><span style="font-family: "New
serif",serif;color:#1D2228;background:white;mso-ansi-language:EN-US"
lang="EN-US">ANISOTROPY OF MAGNETIC SUSCEPTIBILITY ANALYSIS IN
CORES OF TUNAS FORMATION (PERMIAN), CLAROMECÓ BASIN, BUENOS
AIRES, ARGENTINA: IT RELATION WITH DEPOSITIONAL CONDITIONS. </span><span
style="font-family:"New serif",serif;
color:#1D2228;background:white;mso-ansi-language:ES" lang="ES">Febbo
et al. </span><span
style="font-size:10.0pt;font-family:"Helvetica",sans-serif;color:#1D2228"></span></p>
<p class="yiv9431367660ydp3fd7ada8msonormal"
style="margin-bottom:6.0pt; background:white"><span
style="font-family:"New serif",serif;
color:#1D2228;mso-ansi-language:EN-US" lang="EN-US">3)</span><span
style="font-size:7.0pt;font-family:"New
serif",serif;color:#1D2228;mso-ansi-language: EN-US"
lang="EN-US"> </span><span style="font-family: "New
serif",serif;color:#1D2228;background:white;mso-ansi-language:EN-US"
lang="EN-US">THE PERVASIVE SANRAFAELIC REMAGNETIZATION IN
CARBONATES OF THE ARGENTINE PRECORDILLERA. Fazzito et al. </span><span
style="font-size:10.0pt;font-family:"Helvetica",sans-serif;
color:#1D2228;mso-ansi-language:EN-US" lang="EN-US"></span></p>
<p class="yiv9431367660ydp3fd7ada8msonormal"
style="margin-bottom:0cm;margin-bottom: .0001pt;background:white"><span
style="font-family:"New serif",serif;
color:#1D2228;mso-ansi-language:EN-US" lang="EN-US">4)</span><span
style="font-size:7.0pt;font-family:"New
serif",serif;color:#1D2228;mso-ansi-language: EN-US"
lang="EN-US"> </span><span style="font-family: "New
serif",serif;color:#1D2228;background:white;mso-ansi-language:EN-US"
lang="EN-US">VARIATION OF THE EARTH'S MAGNETIC FIELD STRENGTH IN
MEXICO OVER THE LAST THREE MILLENIA. </span><span
style="font-family:"New serif",serif;
color:#1D2228;mso-ansi-language:EN-US" lang="EN-US">Garcia et
al.</span><span
style="font-size:10.0pt;font-family:"Helvetica",sans-serif;
color:#1D2228;mso-ansi-language:EN-US" lang="EN-US"></span></p>
<p class="yiv9431367660ydp3fd7ada8msonormal"
style="margin-bottom:0cm;margin-bottom: .0001pt;background:white"><span
style="font-family:"New serif",serif;
color:#1D2228;mso-ansi-language:EN-US" lang="EN-US">5)</span><span
style="font-size:7.0pt;font-family:"New
serif",serif;color:#1D2228;mso-ansi-language: EN-US"
lang="EN-US"> </span><span style="font-family: "New
serif",serif;color:#1D2228;mso-ansi-language:EN-US"
lang="EN-US">AN INTEGRATED PALEOMAGNETIC SURVEY FROM ZAPICAN
DIKE SWARM (URUGUAY): GEOMAGNETIC AND GEODYNAMIC IMPLICATIONS.
Cervantes et. al</span><span
style="font-size:10.0pt;font-family:"Helvetica",sans-serif;color:#1D2228;mso-ansi-language:EN-US"
lang="EN-US"></span></p>
<p class="yiv9431367660ydp3fd7ada8msonormal"
style="margin-bottom:0cm;margin-bottom: .0001pt;background:white"><span
style="font-family:"New serif",serif;
color:#1D2228;mso-ansi-language:EN-US" lang="EN-US">6)</span><span
style="font-size:7.0pt;font-family:"New
serif",serif;color:#1D2228;mso-ansi-language: EN-US"
lang="EN-US"> </span><span style="font-family: "New
serif",serif;color:#1D2228;mso-ansi-language:EN-US"
lang="EN-US">PLIOCENE PALEOSECULAR VARIATION AND GEOMAGNETIC
EXCURSIONS RECORDED IN CENTRAL AND WESTERN MEXICO.
Gogichaishvili et al.</span><span style="font-size:10.0pt;
font-family:"Helvetica",sans-serif;color:#1D2228;mso-ansi-language:EN-US"
lang="EN-US"></span></p>
<p class="yiv9431367660ydp3fd7ada8msonormal"
style="margin-bottom:6.0pt; background:white"><span
style="font-family:"New serif",serif;
color:#1D2228;mso-ansi-language:EN-US" lang="EN-US">7)</span><span
style="font-size:7.0pt;font-family:"New
serif",serif;color:#1D2228;mso-ansi-language: EN-US"
lang="EN-US"> </span><span style="font-family: "New
serif",serif;color:#1D2228;background:white;mso-ansi-language:EN-US"
lang="EN-US">ROCK MAGNETIC STUDY OF THE CHICXULUB PEAK RING
SEQUENCE - IODP/ICDP EXPEDITION 364 SITE M0077A, YUCATAN
PLATFORM, GULF OF MEXICO. Urrutia-Fucugauchi et al. </span><span
style="font-size:10.0pt;font-family:"Helvetica",sans-serif;
color:#1D2228;mso-ansi-language:EN-US" lang="EN-US"></span></p>
<p class="yiv9431367660ydp3fd7ada8msonormal"
style="margin-bottom:6.0pt; background:white"><span
style="font-family:"New serif",serif;
color:#1D2228;mso-ansi-language:EN-US" lang="EN-US">8)</span><span
style="font-size:7.0pt;font-family:"New
serif",serif;color:#1D2228;mso-ansi-language: EN-US"
lang="EN-US"> </span><span style="font-family: "New
serif",serif;color:#1D2228;background:white;mso-ansi-language:EN-US"
lang="EN-US">A CHARACTERIZATION OF THE SURFICIAL EXPRESSION OF
UPWARD HYDROCARBON MICROSEEPAGE IN WESTERN VENEZUELA, BY
INTEGRATING REMOTE SENSING SPECTRAL ANALYSIS AND ROCK MAGNETIC
DATA. Costanzo Alvarez et al.</span><span
style="font-size:10.0pt;font-family:"Helvetica",sans-serif;color:#1D2228;mso-ansi-language:EN-US"
lang="EN-US"></span></p>
<p class="yiv9431367660ydp3fd7ada8msonormal"
style="margin-bottom:6.0pt; background:white"><span
style="font-family:"New serif",serif;
color:#1D2228;mso-ansi-language:EN-US" lang="EN-US">9)</span><span
style="font-size:7.0pt;font-family:"New
serif",serif;color:#1D2228;mso-ansi-language: EN-US"
lang="EN-US"> </span><span style="font-family:"New
serif",serif;
color:#1D2228;background:white;mso-ansi-language:EN-US"
lang="EN-US">TECTONIC ROTATIONS IN THE NORTHERN PATAGONIAN
CORDILLERA DETERMINED BY PALEOMAGNETIC STUDIES: PRELIMINARY
RESULTS. Milanese et al.</span></p>
<p class="MsoNormal" style="margin-bottom:0cm;margin-bottom:.0001pt"><span
style="font-family:"New
serif",serif;color:#1D2228;background:white;
mso-ansi-language:EN-US" lang="EN-US">10) </span><span
style="font-size:12.0pt;
line-height:107%;font-family:"Times New
Roman",serif;mso-fareast-font-family: "Times New
Roman";mso-ansi-language:EN-US;mso-fareast-language:ES-AR;
mso-bidi-font-weight:bold;mso-bidi-font-style:italic"
lang="EN-US">FOLLOWING THE STEPS OF CHIPA. Tomezzoli et al. <br>
</span></p>
<p class="MsoNormal"
style="margin-bottom:0cm;margin-bottom:.0001pt;line-height:
normal"><span style="font-size:12.0pt;
line-height:107%;font-family:"Times New
Roman",serif;mso-fareast-font-family: "Times New
Roman";mso-ansi-language:EN-US;mso-fareast-language:ES-AR;
mso-bidi-font-weight:bold;mso-bidi-font-style:italic"
lang="EN-US">11)</span><span
style="font-size:12.0pt;mso-fareast-font-family:"Times New
Roman";
mso-bidi-font-family:"Times New
Roman";color:#26282A;mso-ansi-language:EN-US;
mso-fareast-language:ES-AR" lang="EN-US"> 2D MAGNETIC MODELLING
OF TONA ANOMALY AT THE
ARGENTINE CONTINENTAL MARGIN. </span><span
style="font-size:12.0pt;mso-fareast-font-family:
"Times New Roman";mso-bidi-font-family:"Times New
Roman";color:#26282A;
mso-fareast-language:ES-AR">Ana Carolina Pedraza De Marchi,
Marta E. Ghidella,
Juan Francese, Julián Gómez</span><span
style="font-size:12.0pt;mso-fareast-font-family:
"Times New Roman";mso-bidi-font-family:"Times New
Roman";mso-fareast-language:
ES-AR"></span></p>
<p class="MsoNormal" style="margin-bottom:0cm;margin-bottom:.0001pt"><span
style="font-size:12.0pt;
line-height:107%;font-family:"Times New
Roman",serif;mso-fareast-font-family: "Times New
Roman";mso-ansi-language:EN-US;mso-fareast-language:ES-AR;
mso-bidi-font-weight:bold;mso-bidi-font-style:italic"
lang="EN-US">
</span></p>
<span style="font-size:12.0pt;
line-height:107%;font-family:"Times New
Roman",serif;mso-fareast-font-family: "Times New
Roman";mso-ansi-language:EN-US;mso-fareast-language:ES-AR;
mso-bidi-font-weight:bold;mso-bidi-font-style:italic" lang="EN-US">
<p class="MsoNormal"
style="margin-bottom:0cm;margin-bottom:.0001pt;line-height:
normal;background:white"><span
style="font-size:12.0pt;mso-fareast-font-family:
"Times New Roman";mso-bidi-font-family:"Times
New Roman";color:#26282A;
mso-ansi-language:EN-US;mso-fareast-language:ES-AR"
lang="EN-US">12) </span><span
style="font-size:12.0pt;mso-fareast-font-family:"Times
New Roman";
mso-bidi-font-family:"Times New
Roman";color:#1D2228;mso-ansi-language:EN-US;
mso-fareast-language:ES-AR" lang="EN-US">PALEOMAGNETISM AND
40AR/39AR CHRONOLOGY OF
IGNIMBRITES AND LAVA FLOWS, ATACAMA REGION, CENTRAL VOLCANIC
ZONE, NORTHERN
CHILE. L. Brown, B. Singer and M. Barquero-Molina</span></p>
<p class="MsoNormal"
style="margin-bottom:0cm;margin-bottom:.0001pt;line-height:
normal;background:white"><span
style="font-size:12.0pt;mso-fareast-font-family:"Times
New Roman";
mso-bidi-font-family:"Times New
Roman";color:#1D2228;mso-ansi-language:EN-US;
mso-fareast-language:ES-AR" lang="EN-US"></span></p>
</span><span style="font-size:12.0pt;
line-height:107%;font-family:"Times New
Roman",serif;mso-fareast-font-family: "Times New
Roman";mso-ansi-language:EN-US;mso-fareast-language:ES-AR;
mso-bidi-font-weight:bold;mso-bidi-font-style:italic" lang="EN-US">
<h1
style="margin:0cm;margin-bottom:.0001pt;vertical-align:baseline"><span
style="font-size:12.0pt;font-family:"Calibri",sans-serif;mso-ascii-theme-font:
minor-latin;mso-hansi-theme-font:minor-latin;color:#1D2228;mso-ansi-language:
EN-US;font-weight:normal;mso-bidi-font-weight:bold"
lang="EN-US">13) I</span><span
style="font-size:12.0pt;font-family:"Calibri",sans-serif;mso-ascii-theme-font:minor-latin;mso-hansi-theme-font:minor-latin;color:black;mso-ansi-language:
EN-US;font-weight:normal;mso-bidi-font-weight:bold"
lang="EN-US">NTERPLAY BETWEEN MAGNETIC
FABRICS DURING EMPLACEMENT OF THE CALMAYO PLUTON, EASTERN
SIERRAS
PAMPEANAS, ARGENTINA. </span><span style="font-size:12.0pt;
font-family:"Calibri",sans-serif;mso-ascii-theme-font:minor-latin;mso-hansi-theme-font:
minor-latin;color:black;mso-themecolor:text1;mso-ansi-language:EN-US;
font-weight:normal;mso-bidi-font-weight:bold" lang="EN-US">Lucio
Pinotti, Fernando D'Eramo,
Silvana Geuna, Stefania Radice, Manuel Demartis, Joaquín
Coniglio, José María
Tubía ,David Gómez-Ortíz, Jorge Coniglio, José Kostadinoff</span></h1>
</span><br>
<span style="font-size:12.0pt;
line-height:107%;font-family:"Times New
Roman",serif;mso-fareast-font-family: "Times New
Roman";mso-ansi-language:EN-US;mso-fareast-language:ES-AR;
mso-bidi-font-weight:bold;mso-bidi-font-style:italic" lang="EN-US">
<h1
style="margin:0cm;margin-bottom:.0001pt;vertical-align:baseline"><span
style="font-size:12.0pt;font-family:"Calibri",sans-serif;mso-ascii-theme-font:
minor-latin;mso-hansi-theme-font:minor-latin;color:black;mso-themecolor:text1;
mso-ansi-language:EN-US;font-weight:normal;mso-bidi-font-weight:bold"
lang="EN-US">14) ROCK
MAGNETIC CHARACTERIZATION OF A LATE PALEOZOIC REMAGNETIZATION
OF
CAMBRIAN METASEDIMENTS IN THE SIERRA DE MOJOTORO, EASTERN
CORDILLERA,
ARGENTINA. Pablo Franceschinis et al. <span
style="mso-spacerun:yes"></span></span></h1>
</span><br>
<span style="font-size:12.0pt;
line-height:107%;font-family:"Times New
Roman",serif;mso-fareast-font-family: "Times New
Roman";mso-ansi-language:EN-US;mso-fareast-language:ES-AR;
mso-bidi-font-weight:bold;mso-bidi-font-style:italic" lang="EN-US">
<h1
style="margin:0cm;margin-bottom:.0001pt;vertical-align:baseline"><span
style="font-size:12.0pt;font-family:"Calibri",sans-serif;mso-ascii-theme-font:
minor-latin;mso-hansi-theme-font:minor-latin;color:black;mso-themecolor:text1;
mso-ansi-language:EN-US;font-weight:normal;mso-bidi-font-weight:bold"
lang="EN-US">15</span><span
style="font-size:12.0pt;font-family:"Calibri",sans-serif;color:black;mso-themecolor:text1;mso-ansi-language:EN-US;font-weight:normal;mso-bidi-font-weight:
bold" lang="EN-US">) </span><span
style="font-size:12.0pt;font-family:"Calibri",sans-serif;
color:#1D2228;background:white;mso-ansi-language:EN-US;font-weight:normal;
mso-bidi-font-weight:bold" lang="EN-US">CAN MAGNETIC FABRIC
INDICATE THE DIRECTION OF A
GLACIER MOVEMENT? AN EXAMPLE FROM ITARARÉ AND
AQUIDAUNA FORMATIONS, PARANÁ
BASIN, BRAZIL. I. Raposo et al.</span><span
style="font-size:12.0pt;
font-family:"Calibri",sans-serif;color:black;mso-themecolor:text1;mso-ansi-language:
EN-US;font-weight:normal;mso-bidi-font-weight:bold"
lang="EN-US"></span></h1>
</span>
<p class="MsoNormal" style="margin-bottom:0cm;margin-bottom:.0001pt"><span
style="font-size:12.0pt;
line-height:107%;font-family:"Times New
Roman",serif;mso-fareast-font-family: "Times New
Roman";mso-ansi-language:EN-US;mso-fareast-language:ES-AR;
mso-bidi-font-weight:bold;mso-bidi-font-style:italic"
lang="EN-US"><br>
</span></p>
<p class="MsoNormal" style="margin-bottom:0cm;margin-bottom:.0001pt"><span
style="font-size:12.0pt;line-height:107%;font-family:"Times
New Roman",serif; mso-fareast-font-family:"Times New
Roman";mso-fareast-language:ES-AR"><br>
</span></p>
<p class="MsoNormal" style="margin-bottom:0cm;margin-bottom:.0001pt"><span
style="font-size:12.0pt;line-height:107%;font-family:"Times
New Roman",serif; mso-fareast-font-family:"Times New
Roman";mso-fareast-language:ES-AR">Saludos <br>
</span></p>
<span
style="font-size:12.0pt;line-height:107%;font-family:"Times
New Roman",serif; mso-fareast-font-family:"Times New
Roman";mso-fareast-language:ES-AR">Augusto, Cecilia, </span><span
style="font-size:12.0pt;line-height:107%;font-family:"Times
New Roman",serif; mso-fareast-font-family:"Times New
Roman";mso-fareast-language:ES-AR"><span
style="font-size:12.0pt;line-height:107%;font-family:"Times
New Roman",serif; mso-fareast-font-family:"Times New
Roman";mso-fareast-language:ES-AR">Fernando</span> e Irene</span>
<pre class="moz-signature" cols="72">--
Dr. Augusto E. Rapalini
Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires
UBA – CONICET
Universidad de Buenos Aires
Facultad de Ciencias Exactas y Naturales
Departamento de Ciencias Geológicas
Pabellón II Ciudad Universitaria
Intendente Güiraldes 2160 - CP: C1428EHA
Ciudad Autónoma de Buenos Aires
Argentina</pre>
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