Banca de DEFESA: VIRGINIE D'HOUR

Uma banca de DEFESA de DOUTORADO foi cadastrada pelo programa.
DISCENTE: VIRGINIE D'HOUR
DATA: 01/09/2015
HORA: 09:00
LOCAL: Auditório do Departamento de Geofísica-UFRN
TÍTULO:

Medium change monitoring using ambient seismic noise and coda wave interferometry: examples from intraplate NE Brazil and the Mid-Atlantic Ridge.

PALAVRAS-CHAVES:

ambient seismic noise, auto- and cross-correlation, coda wave, interferometry, intraplate, Mid-Atlantic Ridge.

PÁGINAS: 120
GRANDE ÁREA: Ciências Exatas e da Terra
ÁREA: Geociências
RESUMO:

This thesis presents and discusses the results of ambient seismic noise correlation for two different context: intraplate and Mid-Atlantic Ridge. The coda wave interferometry method have also been tested for the intraplate data.

Ambient noise correlation is a method that allows to retrieve the structural response between two receivers from ambient noise records, as if one of the station was a virtual source. It has been largely used in seismology to image the subsurface and to monitor structural changes associated mostly with volcanic eruptions and large earthquakes.

In the intraplate study, we were able to detect localized structural changes related to this small earthquake swarm, which main event is mR 3.7, North-East of Brazil. We also showed that the 1-bit normalization and spectral whitening results on loss of waveform details and that the phase auto-correlation, which is amplitude unbiased, seems to be more sensitive and robust for our analysis of a small earthquake swarm. The analysis of 6 months of data using cross-correlations detect clear medium changes soon after the main event while the auto-correlations detect changes essentially after 1 month. It could be explained by fluid pressure redistribution which can be initiated by hydromechanical changes and opened path ways to shallower depth levels due to later occurring earthquakes.

In the Mid-Atlantic Ridge study, we investigate structural changes associated with a mb 4.9 earthquake in the region of the Saint Paul transform fault. The data have been recorded by a single broadband seismic station located at less than 200 km from the Mid-Atlantic ridge. The results of the phase auto-correlation for a 5-month period, show a strong co-seismic medium change followed by a relatively fast post-seismic recovery. This medium change is likely related to the damages caused by the earthquake’s ground shaking. The healing process (filling of the new cracks) that lasted 60 days can be decomposed in two phases, a fast recovery (70% in ~30 days) in the early post-seismic stage and a relatively slow recovery later (30% in ~30 days).

In the coda wave interferometry study, we monitor temporal changes of the subsurface caused by the small intraplate earthquake swarm mentioned previously. The method was first validated with synthetics data. We were able to detect a 2.5% source dislocation and a 15% decrease of the scatterers’ amount. Then, from the real data, we observed a rapid decorrelation of the seismic coda after the mR 3.7 seismic event. This indicates a rapid change of the subsurface in the fault’s region induced by the earthquake. 

MEMBROS DA BANCA:
Presidente - 1451214 - ADERSON FARIAS DO NASCIMENTO
Interno - 350640 - FRANCISCO HILARIO REGO BEZERRA
Interno - 1863578 - JORDI JULIA CASAS
Externo à Instituição - LUCAS VIEIRA BARROS - UnB
Externo à Instituição - MARCELO SOUSA DE ASSUMPÇÃO - USP