2020
DOI: 10.33958/revig.v41i1.689
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Carta do modelado e das formações superficiais do médio vale do rio Parateí, SP – 1:25.000

Abstract: Republicação da “Carta do Modelado e das Formações Superficiais do Médio Vale do Rio Parateí, SP – 1:25.000” e memorial explicativo, originalmente publicado em “Sedimentologia e Pedologia”, número 9, pelo Instituto de Geografia, Universidade de São Paulo, São Paulo, em 1978. Pesquisa desenvolvida no âmbito do convênio entre o Laboratório de Pedologia e Sedimentologia do Instituto de Geografia / Departamento de Geografia da Faculdade de Filosofia, Letras e Ciências Humanas da Universidade de São Paulo e o Centr… Show more

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“…In Brazil, Pedological and Geomorphological research highlighted the evolution of landforms by defining the autochthonous and allochthonous nature of materials (FEUER, 1956;BIGARELLA et al, 1961;AB'SÁBER, 1962;BENNEMA et al 1962;BIGARELLA et al, 1965;CARVALHO et al, 1969;COUTARD et al, 1978;DIAS FERREIRA et al, 1978). Some criteria were employed to define allochthony and autochthony through a study of superficial formations, such as the presence of stone-lines with or without ferruginous concretions, which would differ from the geological substrate and follow the slope profile, as well as the marked differences in the mineralogical composition or chemical properties of successive horizons, and the presence of buried horizons rich in organic matter and evidencing the presence of paleosols (QUEIROZ NETO, 2001).…”
Section: Pedological Influences In the Modification Of Landformsmentioning
confidence: 99%
“…In Brazil, Pedological and Geomorphological research highlighted the evolution of landforms by defining the autochthonous and allochthonous nature of materials (FEUER, 1956;BIGARELLA et al, 1961;AB'SÁBER, 1962;BENNEMA et al 1962;BIGARELLA et al, 1965;CARVALHO et al, 1969;COUTARD et al, 1978;DIAS FERREIRA et al, 1978). Some criteria were employed to define allochthony and autochthony through a study of superficial formations, such as the presence of stone-lines with or without ferruginous concretions, which would differ from the geological substrate and follow the slope profile, as well as the marked differences in the mineralogical composition or chemical properties of successive horizons, and the presence of buried horizons rich in organic matter and evidencing the presence of paleosols (QUEIROZ NETO, 2001).…”
Section: Pedological Influences In the Modification Of Landformsmentioning
confidence: 99%