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dc.contributor.authorSchuster, Gerard T.
dc.date.accessioned2021-04-20T11:46:59Z
dc.date.available2021-04-20T11:46:59Z
dc.date.issued2016-11-21
dc.identifier.citationSchuster, G. T. (2014). 5. Seismic Interferometry. Encyclopedia of Exploration Geophysics, Q1–1–Q1–41. doi:10.1190/1.9781560803027.entry5
dc.identifier.isbn9781560803010
dc.identifier.isbn9781560803027
dc.identifier.doi10.1190/1.9781560803027.entry5
dc.identifier.urihttp://hdl.handle.net/10754/668877
dc.description.abstractControlled-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.
dc.publisherSociety of Exploration Geophysicists
dc.relation.urlhttps://library.seg.org/doi/10.1190/1.9781560803027.entry5
dc.rightsArchived with thanks to Society of Exploration Geophysicists
dc.title5. Seismic Interferometry
dc.typeBook Chapter
dc.contributor.departmentEarth Science and Engineering Program
dc.contributor.departmentPhysical Science and Engineering (PSE) Division
dc.eprint.versionPost-print
dc.identifier.pagesQ1-1-Q1-41
kaust.personSchuster, Gerard T.


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