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(Referência obtida automaticamente do Web of Science, por meio da informação sobre o financiamento pela FAPESP e o número do processo correspondente, incluída na publicação pelos autores.)

Genetic algorithm inversion of the average 1D crustal structure using local and regional earthquakes

Texto completo
Autor(es):
de Vasconcelos Lopes, Afonso Emidio [1] ; Assumpcao, Marcelo [1]
Número total de Autores: 2
Afiliação do(s) autor(es):
[1] Univ Sao Paulo IAG USP, Inst Astron Geophys & Atmospher Sci, BR-05508090 Sao Paulo - Brazil
Número total de Afiliações: 1
Tipo de documento: Artigo Científico
Fonte: Computers & Geosciences; v. 37, n. 9, p. 1372-1380, SEP 2011.
Citações Web of Science: 4
Resumo

Knowing the best 1D model of the crustal and upper mantle structure is useful not only for routine hypocenter determination, but also for linearized joint inversions of hypocenters and 3D crustal structure, where a good choice of the initial model can be very important. Here, we tested the combination of a simple GA inversion with the widely used HYPO71 program to find the best three-layer model (upper crust, lower crust, and upper mantle) by minimizing the overall P- and S-arrival residuals, using local and regional earthquakes in two areas of the Brazilian shield. Results from the Tocantins Province (Central Brazil) and the southern border of the Sao Francisco craton (SE Brazil) indicated an average crustal thickness of 38 and 43 km, respectively, consistent with previous estimates from receiver functions and seismic refraction lines. The GA + HYPO71 inversion produced correct Vp/Vs ratios (1.73 and 1.71, respectively), as expected from Wadati diagrams. Tests with synthetic data showed that the method is robust for the crustal thickness, Pn velocity, and Vp/Vs ratio when using events with distance up to about 400 km, despite the small number of events available (7 and 22, respectively). The velocities of the upper and lower crusts, however, are less well constrained. Interestingly, in the Tocantins Province, the GA + HYPO71 inversion showed a secondary solution (local minimum) for the average crustal thickness, besides the global minimum solution, which was caused by the existence of two distinct domains in the Central Brazil with very different crustal thicknesses. (C) 2010 Elsevier Ltd. All rights reserved. (AU)

Processo FAPESP: 96/01566-0 - Estudos geofísicos e modelo tectônico dos setores central e sudeste da província Tocantins, Brasil central
Beneficiário:Jesus Antonio Berrocal Gomez
Modalidade de apoio: Auxílio à Pesquisa - Temático
Processo FAPESP: 03/12204-8 - Mecanismos focais e esforços litosféricos no Brasil
Beneficiário:Afonso Emidio de Vasconcelos Lopes
Modalidade de apoio: Bolsas no Brasil - Doutorado Direto
Processo FAPESP: 02/01001-6 - Sismicidade e estrutura crustal em goias.
Beneficiário:Afonso Emidio de Vasconcelos Lopes
Modalidade de apoio: Bolsas no Brasil - Iniciação Científica