Searched for: subject%3A%22Body%255C%2Bwaves%22
(1 - 3 of 3)
van IJsseldijk, J.E. (author), Ruigrok, E. (author), Verdel, A. (author), Weemstra, C. (author)
Global phases, viz. seismic phases that travel through the Earth’s core, can be used to locally image the crust by means of seismic interferometry. This method is known as Global Phase Seismic Interferometry (GloPSI). Traditionally, GloPSI retrieves low-frequency information (up to 1 Hz). Recent studies, however, suggest that there is high...
article 2019
Almagro Vidal, C. (author), van der Neut, J. (author), Verdel, A.R. (author), Hartstra, I.E. (author), Wapenaar, K. (author)
Passive seismic interferometry enables the estimation of the reflection response of the subsurface using passive receiver recordings at the surface from sources located deep in the Earth. Interferometric imaging makes use of this retrieved reflection response in order to study the subsurface. Successful interferometric imaging relies on the...
article 2018
Draganov, D. (author), Campman, X. (author), Thorbecke, J. (author), Verdel, A. (author), Wapenaar, K. (author)
The successful surface waves retrieval in solid-Earth seismology using long-time correlations and subsequent tomographic images of the crust have sparked interest in extraction of subsurface information from noise in the exploration seismology. Subsurface information in exploration seismology is usually derived from body-wave reflections > 1 Hz,...
article 2013