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Publikováno v:
Physics of the Earth and Planetary Interiors. 78:239-244
The anisotropy beneath the North Pyrenean fault, which delineates the boundary between the Eurasian and Iberian plates, is studied from the splitting of SKS- and SKKS-waves recorded at a broad-band station of the NARS array in the western Pyrenees. E
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::88d8bda7057e986102e0613b8f4c967f
https://doi.org/10.1016/0031-9201(93)90158-6
https://doi.org/10.1016/0031-9201(93)90158-6
