2019
DOI: 10.1093/gji/ggz227
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Characterization of crustal structure by comparing reflectivity patterns of wide-angle and near vertical seismic data from the Parnaíba Basin, Brazil

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Cited by 6 publications
(2 citation statements)
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“…The crustal velocity law obtained varies between 5.7 km/s and 7.1 km/s, without any variation from 37 km downwards and it is agree with the global average for platforms given by , the largest difference is the higher velocity at shallower depths up to 12 km observed in our predicted law. Nevertheless, the data available for Brazil (Soares et al, 2006;Lima et al, 2019) shows higher velocities at shallower depths (Figure 4.3b). All bibliography reviewed presents a similar pattern of velocity gradient with the depth; however, the crustal velocities at Cadiz Gulf • The Andes highlands: Considering the thicker crust under the Andes (up to ∼70 km), and the different velocity gradient due to their tectonic evolution (Beck and Zandt, 2002), we calculated another law for this region, considering the global average for orogens from , and active seismic studies in the region (Beck and Zandt, 2002;Oncken et al, 2003;.…”
Section: Sedimentary and Crustal Velocitiesmentioning
confidence: 93%
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“…The crustal velocity law obtained varies between 5.7 km/s and 7.1 km/s, without any variation from 37 km downwards and it is agree with the global average for platforms given by , the largest difference is the higher velocity at shallower depths up to 12 km observed in our predicted law. Nevertheless, the data available for Brazil (Soares et al, 2006;Lima et al, 2019) shows higher velocities at shallower depths (Figure 4.3b). All bibliography reviewed presents a similar pattern of velocity gradient with the depth; however, the crustal velocities at Cadiz Gulf • The Andes highlands: Considering the thicker crust under the Andes (up to ∼70 km), and the different velocity gradient due to their tectonic evolution (Beck and Zandt, 2002), we calculated another law for this region, considering the global average for orogens from , and active seismic studies in the region (Beck and Zandt, 2002;Oncken et al, 2003;.…”
Section: Sedimentary and Crustal Velocitiesmentioning
confidence: 93%
“…• South American platform: we collected Brazilian available data of the central part (Soares et al, 2006) and northeastern region Lima et al (2019); we considered the averages for platforms given by ; and crustal velocity structures from the East European Craton (Starostenko et al, 2013), Siberian…”
Section: Sedimentary and Crustal Velocitiesmentioning
confidence: 99%