The Northern part of line GRANU 9501 shows

• in the SE part of the profile prominent, NW-dipping reflections at 2 s TWT,
• good correlation with line DEKORP 3B/MVE-90,
• structures traceable further to the SE below the Erzgebirge.

The central part of the profile shows

• diffuse reflectivity in upper and middle crust due by nearby granites,
• some few, continuous reflections between 9 - 10 s TWT.

The NW half shows

• NW-dipping reflection events between 1-2 s TWT, => correlate with Vp ca. 6.5 km/s from refraction seismics,
• strong reflection bands between 4.5 - 5.5 s TWT with SE dip.

The Erzgebirge is imaged on the SE half of line 9502

• the SE end of the profile is less reflective in the uppermost crust,
• strong, NW-dipping reflection bands between surface and 4 s TWT,
• base of Norderzgebirge Basin in 1-2 s TWT,
• fault structures separate granulites from Permo-Carboniferous basin,reflective lower crust.