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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.)

Improving C-1 and C-3 empirical Green's functions from ambient seismic noise in NW Iran using RMS ratio stacking method

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Autor(es):
Safarkhani, Mahsa [1] ; Shirzad, Taghi [2]
Número total de Autores: 2
Afiliação do(s) autor(es):
[1] Univ Tehran, Inst Geophys, Tehran 141556466 - Iran
[2] Univ Sao Paulo, Inst Astron Geophys & Atmospher Sci, BR-05508090 Sao Paulo - Brazil
Número total de Afiliações: 2
Tipo de documento: Artigo Científico
Fonte: JOURNAL OF SEISMOLOGY; v. 23, n. 4, p. 787-799, JUL 2019.
Citações Web of Science: 1
Resumo

The retrieval of stable and reliable empirical Green's functions using ambient seismic noise plays a major role when studying the Earth's structure at various scales. High-resolution noise correlation functions are obtained in the NW of Iran by processing techniques including dividing the continuously recorded raw data into short (i.e., 10min) overlapping (i.e., 80%) time windows. We compare four stacking methods (i.e., linear, RMS, RMS ratio, and Nth-root stacking methods) to study robust and stable inter-station empirical Green's functions. Our results indicate that the new RMS ratio method of stacking would be the optimal method to stack coherent signals. In other words, this method tackles problems including low signal-to-noise ratio (hereafter SNR) value, distortion of wave shape, and phase instability/unstable polarity treatment. In addition to noise correlation functions, we propose another strategy for the computation of the empirical Green's functions. In this technique, the cross-correlation of scattered coda waves of the calculated noise correlation functions is performed individually. In addition to coda window length, we also investigate another effective parameter, the geometry of various virtual stations to obtain reliable empirical Green's functions from the scattered coda waves of correlation functions with high SNR. The error of the velocities of Rayleigh wave empirical Green's functions is on the order of approximately 0.6%, when compared to ambient seismic noise and scattered coda waves for a period band range of 3-10s. (AU)

Processo FAPESP: 16/20952-4 - Tomografia de ruído ambiental nas bacias do Pantanal e Paraná
Beneficiário:Taghi Shirzad Iraj
Modalidade de apoio: Bolsas no Brasil - Pós-Doutorado