Fig. 14

Schematic model of continental crust based on Müller (1977). The depth of interfaces are based on the interpretation of the ALP 87 seismic refraction profile J-ED (Maurer & Ansorge, 1992). Averages velocities have been corrected for lithostatic pressure and temperature (see text) using a geothermal gradient as proposed by Okaya et al. (1996) below the Calcareous Alps. Reflection coefficients as calculated by Holliger and Levander (1994) are also shown