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   <subfield code="a">Deep reflection and refraction seismics, integrated with gravimetry, geology and tectonics, have revealed into details the deep structure of the Alps, particularly the big overthrusts and indentations of adriatic crust and mantle slices over and inside the european one. The seismic velocities recorded along the EGT indicate a greater quantity of upper crust, having the missing lower crust been probably absorbed into the mantle. The experimental results by Mengel and Kern (1990) on thev- d relations at high pressures allow finally to find an agreement also with the gravimetric model, and to confirm the interactions mantle-crust.</subfield>
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