Abstract
Continuous recordings of the Earth surface motion by modern seismological networks contain a wealth of information on the structure of the planet and on its temporal evolution. Recent developments shown here make it possible to image the lithosphere with noise only and to detect temporal changes related to inner deformations.
Cite
CITATION STYLE
APA
Campillo, M., Roux, P., & Shapiro, N. M. (2011). Seismic, ambient noise correlation. Encyclopedia of Earth Sciences Series, Part 5, 1230–1236. https://doi.org/10.1007/978-90-481-8702-7_218
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