Open AccessUpper‐mantle seismic structure beneath SE and Central Brazil from P ‐ and S ‐wave regional traveltime tomography
Author(s) -
Rocha Marcelo Peres,
Schimmel Martin,
Assumpção Marcelo
Publication year - 2011
Publication title -
geophysical journal international
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0956-540X
DOI - 10.1111/j.1365-246x.2010.04831.x
Subject(s) - geology , craton , seismology , lithosphere , intraplate earthquake , mantle (geology) , seismic tomography , anomaly (physics) , structural basin , induced seismicity , tectonics , geophysics , paleontology , physics , condensed matter physics
SUMMARY We present models for the upper‐mantle velocity structure beneath SE and Central Brazil using independent tomographic inversions of P ‐ and S ‐wave relative arrival‐time residuals (including core phases) from teleseismic earthquakes. The events were recorded by a total of 92 stations deployed through different projects, institutions and time periods during the years 1992–2004. Our results show correlations with the main tectonic structures and reveal new anomalies not yet observed in previous works. All interpretations are based on robust anomalies, which appear in the different inversions for P ‐ and S ‐waves. The resolution is variable through our study volume and has been analyzed through different theoretical test inversions. High‐velocity anomalies are observed in the western portion of the São Francisco Craton, supporting the hypothesis that this Craton was part of a major Neoproterozoic plate (San Franciscan Plate). Low‐velocity anomalies beneath the Tocantins Province (mainly fold belts between the Amazon and São Francisco Cratons) are interpreted as due to lithospheric thinning, which is consistent with the good correlation between intraplate seismicity and low‐velocity anomalies in this region. Our results show that the basement of the Paraná Basin is formed by several blocks, separated by suture zones, according to model of Milani & Ramos. The slab of the Nazca Plate can be observed as a high‐velocity anomaly beneath the Paraná Basin, between the depths of 700 and 1200 km. Further, we confirm the low‐velocity anomaly in the NE area of the Paraná Basin which has been interpreted by VanDecar et al. as a fossil conduct of the Tristan da Cunha Plume related to the Paraná flood basalt eruptions during the opening of the South Atlantic.