<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>Quaternary sea levels of the Brazilian coast : recent progress</dc:title>
  <dc:creator>Suguio, K.</dc:creator>
  <dc:creator>/Martin, Louis</dc:creator>
  <dc:creator>Flexor, J.M.</dc:creator>
  <dc:subject>NIVEAU MARIN</dc:subject>
  <dc:subject>CLIMAT</dc:subject>
  <dc:subject>VARIATION</dc:subject>
  <dc:subject>LIGNE DE RIVAGE</dc:subject>
  <dc:subject>TRANSGRESSION</dc:subject>
  <dc:subject>REGRESSION</dc:subject>
  <dc:subject>QUATERNAIRE</dc:subject>
  <dc:subject>HOLOCENE</dc:subject>
  <dc:subject>PLAINE COTIERE</dc:subject>
  <dc:description>Les auteurs pr&#xE9;sentent une &#xE9;tude des variations du niveau relatif de la mer au cours du Quaternaire sur la c&#xF4;te orientale du Br&#xE9;sil, de l'Etat Alagoas &#xE0; celui du Rio Grande do Sul. Ils montrent &#xE9;galement que les variations du niveau de la mer et du climat ont jou&#xE9; un r&#xF4;le tr&#xE8;s important dans la formation des plaines c&#xF4;ti&#xE8;res br&#xE9;siliennes</dc:description>
  <dc:date>1988</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:25773</dc:identifier>
  <dc:identifier>fdi:25773</dc:identifier>
  <dc:identifier>Suguio K., Martin Louis, Flexor J.M.. Quaternary sea levels of the Brazilian coast : recent progress. 1988, 11 (3),  203-208</dc:identifier>
  <dc:language>EN</dc:language>
</oai_dc:dc>
