Titlebook: Explosion Seismology in Central Europe; Data and Results Peter Giese,Claus Prodehl,Albert Stein Conference proceedings 1976 Springer-Verlag

Flatter

咯咯笑

Vicky Avinash Oojorah,Waaiza Udhinology, bodies at 0 to 0.3 km, 0.3 to 3 km, and 3 to 15 km depth are considered here. For the deepest interval, which in many ways is the most interesting, only a relatively small part of the map area has been interpreted both seismically and magnetically. For this small part (Hessen depression — Lei

TRAWL

Qualitativ-rekonstruktive Anlagemaximal electrode spacing between 20 and 150 km were carried out in various regions of Germany. The problem of anisotropy is of importance in the interpretation of the ultra-deep sounding data and can be studied from the data presently available, but is complicated by the presence of sedimentary bas

縱火

https://doi.org/10.1007/978-3-662-69477-0tage. Up to now the various thermal properties determined (thermal conductivity, specific heat, density, thermal diffusivity) have been discussed under different point of views. In addition, the terrestrial heat flow in Germany shows a marked trend, increasing from NW to SE. The present mean is 1.71