Time-space subsurface monitoring using seismic ambient noise
21/09/2022
IPGP - Îlot Cuvier
11:00
Séminaires Géosciences Marines
Salle 1400
Peng Guo
CSIRO, Australia
Seismic ambient noise recorded by the ocean bottom nodes (OBNs) in the Gorgon gas field, Western Australia is used to compute time-lapse seafloor models. The extracted hourly cross-correlation (CC) functions of 0.1 – 1 Hz contain mainly Scholte waves with very high signal to noise ratio. The conventional time-lapse analysis suggests relative velocity variations (dv/v) up to 1% assuming a spatially homogeneous dv/v, with a likely 24-hour cycling pattern. With high-resolution baseline models from full waveform inversion of Scholte waves, we propose a wave-equation based double-difference inversion method using differential arrival times for localizing the time-lapse dv/v in the heterogeneous subsurface in depth. The time-lapse velocity models show velocity increase/decrease patterns in agreement with that from conventional analysis, with more notable changes at the shallower depths. We show the feasibility of using ambient noise for quantitative 4-D monitoring of subsurface property changes.
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Topic: Marine Geosciences Seminar - Peng Guo - September 21st
Time: Sep 21, 2022 11:00 AM Paris
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