<?xml version="1.0" encoding="ISO-8859-1"?><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
<front>
<journal-meta>
<journal-id>0016-7169</journal-id>
<journal-title><![CDATA[Geofísica internacional]]></journal-title>
<abbrev-journal-title><![CDATA[Geofís. Intl]]></abbrev-journal-title>
<issn>0016-7169</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geofísica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0016-71692025000101417</article-id>
<article-id pub-id-type="doi">10.22201/igeof.2954436xe.2025.64.1.1747</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Geoelectric Subsurface Characterization in the Emerged Portion of the Barra Falsa Channel using the Ground Conductivity Meter (LIN-EM), Bojuru, RS, Brazil]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Lima]]></surname>
<given-names><![CDATA[José Pedro Rebés]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Corrêa]]></surname>
<given-names><![CDATA[Iran Carlos Stalliviere]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Weschenfelder]]></surname>
<given-names><![CDATA[Jair]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Hansen]]></surname>
<given-names><![CDATA[Marco Antonio Fontoura]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Gruber]]></surname>
<given-names><![CDATA[Nelson Luis Sambaqui]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Moreira]]></surname>
<given-names><![CDATA[Cesar Augusto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Bortolin]]></surname>
<given-names><![CDATA[Eduardo Calixto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidade Federal do Pampa  ]]></institution>
<addr-line><![CDATA[Caçapava do Sul RS]]></addr-line>
<country>Brazil</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidade Federal do Rio Grande do Sul  ]]></institution>
<addr-line><![CDATA[Porto Alegre RS]]></addr-line>
<country>Brazil</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidade Estadual Paulista  ]]></institution>
<addr-line><![CDATA[Rio Claro SP]]></addr-line>
<country>Brazil</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>03</month>
<year>2025</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>03</month>
<year>2025</year>
</pub-date>
<volume>64</volume>
<numero>1</numero>
<fpage>1417</fpage>
<lpage>1435</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692025000101417&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692025000101417&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692025000101417&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Geophysical investigation in the coastal region of the emerged portion of Barra Falsa, Bojuru, RS, Brazil, provided valuable information about the depositional evolution and paleoenvironmental changes that occurred during the Quaternary period. The combination of electromagnetic surveys, analysis of stratigraphic wells, 3.5 kHz reflection seismic and previous geological data allowed for a comprehensive characterization of sedimentary environments associated with sea-level fluctuations. Electromagnetic surveys using the LIN-EM method with the Geonics EM34TM system revealed different conductivity responses in the subsurface, which could be interpreted in relation to depositional events. Five depth intervals were identified and related to specific events, such as the closure of the Barra Falsa channel, estuarine infilling, and channel drowning during marine transgressions. Furthermore, the comparison of the results of electromagnetic surveys with data from stratigraphic wells allowed calibration of indirect data. This multidisciplinary approach highlights the importance of integrating geophysical and geological techniques to reconstruct coastal environment evolution over time. This study provides a detailed insight into paleoenvironmental and depositional changes on the coast of Bojuru, demonstrating how these techniques can significantly contribute to future research and the sustainable management of coastal areas. The knowledge gained here is essential for understanding the dynamics of coastal zones and the influences of sea-level variations in the Southern region of Brazil.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La investigación geofísica en la región costera de la porción emergida de Barra Falsa, Bojuru, RS, Brasil, proporcionó información valiosa sobre la evolución deposicional y los cambios paleoambientales que ocurrieron durante el período Cuaternario. La combinación de estudios electromagnéticos, análisis de pozos estratigráficos, sísmica de reflexión de 3.5 kHz y datos geológicos previos permitió una caracterización integral de los entornos sedimentarios asociados con las fluctuaciones del nivel del mar. Los estudios electromagnéticos utilizando el método LIN-EM con el sistema Geonics EM34TM revelaron diferentes respuestas de conductividad en el subsuelo, que pudieron interpretarse en relación con eventos deposicionales. Se identificaron cinco intervalos de profundidad y se relacionaron con eventos específicos, como el cierre del canal Barra Falsa, el relleno estuarino y el ahogamiento del canal durante las transgresiones marinas. Además, la comparación de los resultados de los estudios electromagnéticos con los datos de pozos estratigráficos permitió la calibración de datos indirectos. Este enfoque multidisciplinario destaca la importancia de integrar técnicas geofísicas y geológicas para reconstruir la evolución del entorno costero a lo largo del tiempo. Este estudio proporciona una visión detallada de los cambios paleoambientales y deposicionales en la costa de Bojuru, demostrando cómo estas técnicas pueden contribuir significativamente a investigaciones futuras y a la gestión sostenible de áreas costeras. El conocimiento adquirido aquí es esencial para comprender la dinámica de las zonas costeras y las influencias de las variaciones del nivel del mar en la región del sur de Brasil.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Coastal Evolution]]></kwd>
<kwd lng="en"><![CDATA[Sea-level fluctuations]]></kwd>
<kwd lng="en"><![CDATA[Stratigraphy]]></kwd>
<kwd lng="en"><![CDATA[Paleochannels]]></kwd>
<kwd lng="en"><![CDATA[LIN-EM Method]]></kwd>
<kwd lng="es"><![CDATA[Evolución Costera]]></kwd>
<kwd lng="es"><![CDATA[Fluctuaciones del nivel del mar]]></kwd>
<kwd lng="es"><![CDATA[Estratigrafía]]></kwd>
<kwd lng="es"><![CDATA[Paleocanales]]></kwd>
<kwd lng="es"><![CDATA[Método LIN-EM]]></kwd>
</kwd-group>
</article-meta>
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