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This document reviews seismic interferometry and ambient noise tomography in the British Isles. It discusses how seismic interferometry can be used to extract useful information about subsurface structures from ambient seismic noise. One application is ambient noise tomography (ANT), which uses surface waves extracted from ambient vibrations to image seismic velocity variations. The document presents the first surface wave group velocity maps of the Scottish Highlands created using only ambient seismic nois

Author

Ridho Destawan

Language

EN