P. Matte et al., GEODYNAMIC MODEL AND AR-39 AR-40 DATING FOR THE GENERATION AND EMPLACEMENT OF THE HIGH-PRESSURE (HP) METAMORPHIC ROCKS IN SW URALS/, Comptes rendus de l'Academie des sciences. Serie 2, Mecanique, physique, chimie, sciences de l'univers, sciences de la terre, 317(12), 1993, pp. 1667-1674
The Urals are a long (3,000 x 200 to 400 km) Paleozoic belt separating
Europe from Asia, characterized by a narrow strip of low temperature/
high pressure (LT/HP) metamorphic rocks outcropping along a major ocea
nic suture, the Main Uralian Fault. We have dated the HP metamorphism
in the southwestern Urals by Ar-39/Ar-40 On phengites at 380 Ma. We pr
opose that it was generated during eastward subduction of the East Eur
opean Paleozoic passive margin below the oceanic mantle during the Dev
onian. The HP rocks were later exhumed (380 to 250 Ma) by the combinat
ion of westward thrusting and eastward normal faulting on the Main Ura
lian Fault.