Investigation of the 600-km discontinuity under France through travel-time and amplitude anomalies

Details Investigation of the 600-km discontinuity under France through travel-time and amplitude anomalies Investigation of the 600-km discontinuity under France through travel-time and amplitude anomalies

May 1974

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1974pepi....8..269m&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 8, Issue 3, p. 269-276.

Physics

1

Scientific paper

In this paper, we give a model of the 600-km discontinuity under France,
which explains large travel-time and amplitude anomalies on teleseisms
as recorded in the French network. It features a large descent from the
Ardennes to the Pyrénées, of which tectonic implications
are discussed.

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