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(Reference retrieved automatically from Web of Science through information on FAPESP grant and its corresponding number as mentioned in the publication by the authors.)

Upper-mantle seismic structure beneath SE and Central Brazil from P- and S-wave regional traveltime tomography

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Author(s):
Rocha, Marcelo Peres [1] ; Schimmel, Martin [2] ; Assumpcao, Marcelo [3]
Total Authors: 3
Affiliation:
[1] Univ Brasilia, Inst Geosci, Brasilia, DF - Brazil
[2] CSIC, Inst Earth Sci Jaume Almera, Barcelona - Spain
[3] Univ Sao Paulo, Dept Geophys, IAG, Sao Paulo - Brazil
Total Affiliations: 3
Document type: Journal article
Source: Geophysical Journal International; v. 184, n. 1, p. 268-286, JAN 2011.
Web of Science Citations: 34
Abstract

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 Sao 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 Sao 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 Parana 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 Parana Basin, between the depths of 700 and 1200 km. Further, we confirm the low-velocity anomaly in the NE area of the Parana Basin which has been interpreted by VanDecar et al. as a fossil conduct of the Tristan da Cunha Plume related to the Parana flood basalt eruptions during the opening of the South Atlantic. (AU)