Seismic tomography

Seismic tomography or seismotomography is a technique for imaging the subsurface of the Earth with seismic waves produced by earthquakes or explosions. P-, S-, and surface waves can be used for tomographic models of different resolutions based on seismic wavelength, wave source distance, and the seismograph array coverage.^[1] The data received at seismometers are used to solve an inverse problem, wherein the locations of reflection and refraction of the wave paths are determined. This solution can be used to create 3D images of velocity anomalies which may be interpreted as structural, thermal, or compositional variations. Geoscientists use these images to better understand core, mantle, and plate tectonic processes.

^ Nolet, G. (1987-01-01). "Seismic wave propagation and seismic tomography". In Nolet, Guust (ed.). Seismic Tomography. Seismology and Exploration Geophysics. Springer Netherlands. pp. 1–23. doi:10.1007/978-94-009-3899-1_1. ISBN 978-90-277-2583-7.

[:0-1] Nolet, G. (1987-01-01). "Seismic wave propagation and seismic tomography". In Nolet, Guust (ed.). Seismic Tomography. Seismology and Exploration Geophysics. Springer Netherlands. pp. 1–23. doi:10.1007/978-94-009-3899-1_1. ISBN 978-90-277-2583-7.

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