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2. TRANSALP SEISMIC PROFILE AND CROP-1A SUBPROJECT

Author

CASTELLARIN A, CANTELLI L, BERTELLI L, BORRINI D, FANTONI R, SELLA M, MAZZOTTI A, SELLI L, BERNABINI M, LAMMERER B, LUESCHEN E, GEBRANDE H, MILLAHN K, GRASSL H, NEUBAUER F, ONCKEN O, STILLER M., NICOLICH, RINALDO, SCROCCA D., DOGLIONIC., INNOCENTI F., MANETTI K., MAZZOTTI A., BERTELLI L., BURBI L., D'OFFIZI S., Castellarin, A, Cantelli, L, Bertelli, L, Borrini, D, Fantoni, R, Sella, M, Nicolich, Rinaldo, Mazzotti, A, Selli, L, Bernabini, M, Lammerer, B, Lueschen, E, Gebrande, H, Millahn, K, Grassl, H, Neubauer, F, Oncken, O, and Stiller, M.

Published
2003

3. European Orogenic Processes. Research Transects the Eastern Alps

Author

GEBRANDE H., LUESCHEN E., CASTELLARIN A., FANTONI R., LAMMERER B., NEUBAUER F., MILLAHN K., BERTELLI L., NICOLICH, RINALDO, Gebrande, H., Lueschen, E., Castellarin, A., Fantoni, R., Lammerer, B., Neubauer, F., Millahn, K., Bertelli, L., and Nicolich, Rinaldo

Published
2001

4. TRANSALP- deep crustal Vibrosels and explosive seismic profiling in the Eastern Alps

Author

Lüschen, E., Borrini, D., Gebrande, H., Lammerer, B., Millahn, K., Neubauer, F., Nicolich, R., TRANSALP Working Group, 3.1 Lithosphere Dynamics, 3.0 Geodynamics and Geomaterials, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, 2.2 Geophysical Deep Sounding, 2.0 Physics of the Earth, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, and 2.4 Seismology, 2.0 Physics of the Earth, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum

Subjects
Graben, Tectonics, Geophysics, Seismic vibrator, Penninic, Dolomite, Anticline, Crust, 550 - Earth sciences, Seismology, Geology, Earth-Surface Processes, Nappe
Abstract

The TRANSALP consortium, comprising institutions from Italy, Austria and Germany, carried out deep seismic reflection measurements in the Eastern Alps between Munich and Venice in 1998, 1999 and 2001. In order to complement each other in resolution and depth range, the Vibroseis technique was combined with simultaneous explosive source measurements. Additionally, passive cross-line recording provided three-dimensional control and alternative north–south sections. Profits were obtained by the combination of the three methods in sectors or depths where one method alone was less successful. The TRANSALP sections clearly image a thin-skinned wedge of tectonic nappes at the northern Alpine front zone, unexpected graben or half-graben structures within the European basement, and, thick-skinned back-thrusting in the southern frontal zone beneath the Dolomite Mountains. A bi-vergent structure at crustal scale is directed from the Alpine axis to the external parts. The Tauern Window obviously forms the hanging wall ramp anticline above a southward dipping, deep reaching reflection pattern interpreted as a tectonic ramp along which the Penninic units of the Tauern Window have been up-thrusted. The upper crystalline crust appears generally transparent. The lower crust in the European domain is characterized by a 6–7 km thick laminated structure. On the Adriatic side the lower crust displays a much thicker or twofold reflective pattern. The crustal root at about 55 km depth is shifted around 50 km to the south with respect to the main Alpine crest.

Published
2006

5. First deep seismic reflection images of the Eastern Alps reveal giant crustal wedges and transcrustal ramps

Author

Gebrande, H., Lüeschen, E., Bopp, M., Bleibinhaus, F., Lammerer, B., Oncken, O., Stiller, M., Kummerow, J., Kind, R., Millahn, K., Grassl, H., Franz Neubauer, Bertelli, L., Borrini, D., Fantoni, R., Pessina, C., Sella, M., Castellarin, A., Nicolich, R., Mazzotti, A., and Bernabini, M.

Subjects
Continental crust, Continental structures, Seismic methods, Continental contractional orogenic belts

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