The newly-defined seismo genic tones in the Alpine-Carpathian-pannonia
n (ALCAPA) junction area are correlated with: (1) Paleoalpine deep-sea
ted suture zones, either oceanic or intracontinental, (2) Neoalpine wr
ench-fault zones following some sutures, and (3) original thrust plane
s reactivated as low-angle extensional normal faults. 1-The principal
West-Carpathian Paleoalpine sutures, from north to south, are: the Pen
ninic-Vahic oceanic suture originated during the Late Cretaceous, the
Certovica intracontinental suture between the Tatric and Veporic thick
-skinned sheets locked some 90 Ma ago, and the Meliatic oceanic suture
formed in the Late Jurassic, closely related to the Igal-Bukk Zone. T
hese suture zones were partly reactivated during the Late Tertiary and
represent weakened zones in the modern upper crust. The concentration
of important earthquake epicenters correlates well with these weakene
d belts which serves as a base for the new seismogenic model of the ar
ea. 2-The most important wrench fault zone is situated between the Eas
tern Alps and Western Carpathians. It reflects the Miocene extrusion o
f the ALCAPA lithospheric fragment from the Alpine domain as its north
western boundary. The NE-SW trending wrench fault zone is represented
by the Mur-Murz-Leitha and Povazie fault systems. The zone is well exp
ressed by flower structures in many seismic lines. 3-The Miocene back-
are extension driven by the subduction pull in front of the Carpathian
orogen and mantle updoming in the Pannonian domain reactivated origin
al Paleoalpine thrusts as crustal detachment planes. In the Danube Bas
in area, these are accompanied by numerous important faults visible in
seismic sections, e.g. the Repce, Raba, Sladkovicovo and Mojmirovce f
ault systems. The extension regime consequences of the core-mountains
uplift during isostatic inversion from the Pliocene are visible in sei
smic section 2T - along the Certovica Zone as strong reflector branche
s. They represent former suture rejuvenated into younger low angle nor
mal faults.