Upper Quaternary sedimentation and hillslope evolution; southeastern Brazilian Plateau

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ID: 296746
1984
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Abstract
Morphostratigraphic evidence indicates that sediment sources and relative rates of erosion over slopes have changes with time. The pattern of change seems to be more compatible with the variable runoff source models than with Horton9s infiltration theory of surface runoff. Older deposits were reworked by successive denudational episodes, resulting in the reshaping of the landforms; erosional discontinuities dominate within the stratigraphic sequences, and stonelines occur at more than one level.--Modified journal abstract.
Reference Key
openalex_W2331893218 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Maria Regina Mousinho de Meis, J. R. d. S. d. Moura
Journal american journal of science
Year 1984
DOI
10.2475/ajs.284.3.241
URL
https://doi.org/10.2475/ajs.284.3.241
Keywords Keywords not found

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