Distribuição sedimentar da lagoa rodrigo de freitas através de sísmica de alta resolução

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Abstract

The Rodrigo de Freitas Lagoon (Rio de Janeiro State) sediments and bottom characteristics were analyzed using high-resolution (10 kHz) sub-bottom profles associated with particle size analyses of 44 bottom sediment samples. Four types of echo-characters were identifed revealing the strong relation with the particle size distribution and bottom morphology. In areas of acoustic penetration, the basement delineates buried sugar-loaf hills and inflled-valley features. The total sediment thickness can reach as much as 16 meters along the paleovalleys, which are aligned in a NE-SW direction, parallel to the regional basement orientation observed on the coastal massifs. There is a predominance of organic rich muddy sediments, inflling the paleovalleys which are the main sites of shallow gas occurrences within the lagoonal sediments. © 2011 Sociedade Brasileira de Geofísica.

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Neto, J. A. B., Silva, C. G., Dias, G. T. de M., & da Fonseca, E. M. (2011). Distribuição sedimentar da lagoa rodrigo de freitas através de sísmica de alta resolução. Revista Brasileira de Geofisica, 29(1), 187–195. https://doi.org/10.1590/S0102-261X2011000100013

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