1. Seismic Interferometry

Abstract
Controlled-source interferometry and ambient-noise interferometry are becoming important tools in earth science. Ambient-noise interferometry is already one of the most important methods for obtaining high-resolution imaging of the crust and upper mantle from dense continent-sized arrays. It also is valuable for estimating the temporal changes in bulk properties of the earth after a large tectonic event. Additional applications include landslide monitoring, temporal changes in the moon's velocity variations, and time-lapse changes in volcanic environments.

Citation
Schuster, G. T. (2014). 5. Seismic Interferometry. Encyclopedia of Exploration Geophysics, Q1–1–Q1–41. doi:10.1190/1.9781560803027.entry5

Publisher
Society of Exploration Geophysicists

DOI
10.1190/1.9781560803027.entry5

Additional Links
https://library.seg.org/doi/10.1190/1.9781560803027.entry5

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