Abstract
The gold and tin-bearing alluvial placers of the Brazilian Amazon high terrains constitute a remarkable record of the environmental changes which occurred in the region during the Quaternary. The deposits are typically immature, and have been formed by mass movements under semi-arid climate. They are clearly older than the last rain forest spreading, and may be attributed to cyclic episodes which have been correlated to the Pleistocene glaciations. These interpretations are highlighted by the discovery of abundant polished stone artifacts which have been preserved within Pleistocene deposits. -from Author
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CITATION STYLE
Veiga, A. T. C. (1991). Paleoenvironmental and archeological significance of alluvial placers of the Brazilian Amazon. Boletim IG - Universidade de Sao Paulo, Instituto de Geociencias, (Spec.Pub.8), 213–222. https://doi.org/10.11606/issn.2317-8078.v0i8p213-222
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