Main Uralian thrust and main Uralian normal fault: non-extensional Palaeozoic high-P rock exhumation, oblique collision, and normal faulting in the Southern Urals

The crustal architecture of the Southern Urals is dominated by an orogenic wedge thrusted westward upon the subducted East European continental margin. The N-S trending wedge constitutes an antiformal stack composed mainly of the high-P Maksyutov Complex, the overlying Suvanyak Complex and the allochthonous synformal Zilair flysch further west. These tectono-metamorphic: units are separated by tectonic contacts and record discontinously decreasing metamorphic conditions from bottom to top. In the east, the E-dipping Main Uralian Normal Fault cross-cuts the metamorphic: footwall and juxtaposes the non metamorphic Magnitogorsk island are. This syncollisional normal fault compensated crustal thickening and exhumation of the high-P rocks. Orogenic shortening was accommodated by the Main Uralian Thrust, a W-vergent crustal-scale shear zone at the base of the wedge. Geological investigations and reflection seismics (URSEIS '95) argue in favour of a geodynamic evolution integrating subduction and basal accretion of high-P rocks during sinistral oblique thrusting along the Main Uralian Thrust and coeval normal-faulting along the Main Uralian Normal Fault.