A natural and controlled source seismic profile through the Eastern Alps: TRANSALP

GFZ Potsdam, Telegrafenberg, 14473 Potsdam, Germany; Freie Universität Berlin, Fachrichtung Geophysik, Malteser Str. 74-100, 12249 Berlin, Germany; Institut für Geowissenschaften, Universität Potsdam, POB 601553, 14415 Potsdam, Germany
Earth and Planetary Science Letters (Impact Factor: 4.72). 08/2004; DOI: 10.1016/j.epsl.2004.05.040

ABSTRACT The combined passive and active seismic TRANSALP experiment produced an unprecedented high-resolution crustal image of the Eastern Alps between Munich and Venice. The European and Adriatic Mohos (EM and AM, respectively) are clearly imaged with different seismic techniques: near-vertical incidence reflections and receiver functions (RFs). The European Moho dips gently southward from 35 km beneath the northern foreland to a maximum depth of 55 km beneath the central part of the Eastern Alps, whereas the Adriatic Moho is imaged primarily by receiver functions at a relatively constant depth of about 40 km. In both data sets, we have also detected first-order Alpine shear zones, such as the Helvetic detachment, Inntal fault and Sub-Tauern ramp in the north. Apart from the Valsugana thrust, receiver functions in the southern part of the Eastern Alps have also observed a north dipping interface, which may penetrate the entire Adriatic crust [Adriatic Crust Interface (ACI)]. Deep crustal seismicity may be related to the ACI. We interpret the ACI as the currently active retroshear zone in the doubly vergent Alpine collisional belt.

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