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Closed depressions in karstic-quartzitic relief, Ribeirão Santana basin, mid-valley of the Paraíba do Sul river
Karstic features generally develop in carbonatic rocks, but can also occur in siliciclastic rocks, as quartzites. The present research aims to create superficial morphology mapping and reconnaissance of karstic area deposits in quartzitic rocks. The study was developed in the hydrographic basin of t...
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Médium: | Online |
Jazyk: | Português |
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Universidade Federal do Rio de Janeiro
2006
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On-line přístup: | https://revistas.ufrj.br/index.php/aigeo/article/view/6619 |
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