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		<label>lattes: 7888258901938956 1 CremonRossZani:2012:GêEvGe</label>
		<citationkey>CremonRossZani:2012:GêEvGe</citationkey>
		<title>Gênese e evolução geomorfológica do megaleque Demini (norte da Amazônia) baseado na análise morfoestrutural e hidroperíodo</title>
		<project>FAPESP (2010/09484-2)</project>
		<year>2012</year>
		<secondarytype>PRE CN</secondarytype>
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		<author>Cremon, Édipo Henrique,</author>
		<author>Rossetti, Dilce de Fátima,</author>
		<author>Zani, Hiran,</author>
		<resumeid></resumeid>
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		<group></group>
		<group>DSR-OBT-INPE-MCTI-GOV-BR</group>
		<affiliation></affiliation>
		<affiliation>Instituto Nacional de Pesquisas Espaciais (INPE)</affiliation>
		<electronicmailaddress>edipocremon@yahoo.com.br</electronicmailaddress>
		<electronicmailaddress>rossetti@dsr.inpe.br</electronicmailaddress>
		<electronicmailaddress>hzani@dsr.inpe.br</electronicmailaddress>
		<e-mailaddress>edipocremon@yahoo.com.br</e-mailaddress>
		<conferencename>Simpósio Nacional de Geomorfologia (SINAGEO), 9</conferencename>
		<conferencelocation>Rio de Janeiro</conferencelocation>
		<date>21-24 de Outubro de 2012</date>
		<booktitle>Anais</booktitle>
		<tertiarytype>Resumo Estendido</tertiarytype>
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		<keywords>megaleque Demini, Amazônia, hidroperíodo, Demini megafan, Amazonia, hydroperiod.</keywords>
		<abstract>O objetivo desse trabalho foi de realizar a analise morfoestrutural do megaleque Demini, norte da Amazônia, e verificar suas possíveis relações com áreas alagadas, visando estabelecer um modelo evolutivo geomorfológico. Para isso, baseou-se na análise morfológica de hidroperíodo e interpretação de anomalias e lineamentos morfoestruturais. Conclui-se que subsidência regional criou depressão com subsequente preenchimento sedimentar e formação do sistema deposicional com extensa área alagável. ABSTRACT: The aim of this work was to perform the Demini megafan morphostructural analysis, northern Amazonia, and verify their possible relationships with wetlands, to establish a model geomorphological evolution. For this, it was based on morphological analysis and interpretation of hydroperiod and morphostructural lineaments. The data indicated that regional subsidence created depression with subsequent formation of sedimentary fill by megafan with extensive flooded area.</abstract>
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		<language>pt</language>
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