2014
DOI: 10.5327/z2317-4889201400020007
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Estratigrafia e estrutura do Cerro do Jarau: nova proposta

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Cited by 7 publications
(11 citation statements)
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“…The negative anomaly in the central area is slightly larger than the proposed laminated sandstone unit in Sánchez et al. (), and the positive circular anomaly begins to show up in the homogeneous sandstone domain, reaching out to the region of basaltic units. Larger density values are expected for the basaltic unit anyway, but based on the density values calculated for rock samples of the structure, the presence of Serra Geral basalts located beneath silicified sandstone bodies is suggested, being this transition expressed in the circular positive anomaly observed.…”
Section: Discussionmentioning
confidence: 61%
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“…The negative anomaly in the central area is slightly larger than the proposed laminated sandstone unit in Sánchez et al. (), and the positive circular anomaly begins to show up in the homogeneous sandstone domain, reaching out to the region of basaltic units. Larger density values are expected for the basaltic unit anyway, but based on the density values calculated for rock samples of the structure, the presence of Serra Geral basalts located beneath silicified sandstone bodies is suggested, being this transition expressed in the circular positive anomaly observed.…”
Section: Discussionmentioning
confidence: 61%
“…) proposed by Sánchez et al. (). It should first be noted that the limit between the sandstone formation in the center and the other sandstone that surrounds it is only inferred due to lack of outcrops, as in the case of the limit between Guará and Botucatu sandstones in the geological map proposed by Crósta et al.…”
Section: Discussionmentioning
confidence: 97%
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