RUPTURE PLANES OF THE GAZLI EARTHQUAKES DEDUCED FROM LOCAL STRESS TENSOR CALCULATION AND GEODETIC DATA INVERSION - GEOTECTONIC IMPLICATIONS

Three major earthquakes (with M(s) greater than or equal to 7) were cl ustered in space and time (1976-1984) near Gazli, Uzbekistan, without reported evidence for fault scarps. To constrain the kinematics of the seismic sequence, we invert both focal mechanism solutions of the mai nshocks and major aftershocks and vertical surface displacements assoc iated with the three major shocks. For seven M > 4 earthquakes that oc curred in the 1976-1984 period, we find that all the focal mechanisms agree with a single stress tenser. One of the mechanical implications of this mathematical solution is the choice of the seismic fault plane . The 1976 earthquake fracture planes are well constrained by the stre ss tensor to be striking E-W and ENE-WSW and dipping to the south and the NNW respectively. From stress tensor inversion alone, it is imposs ible to determine if the fracture plane of the 1984 event dips to the SE or to the NW. Coseismic vertical surface displacements allow us to infer possible fault plane orientations of the 1976 and 1984 events. T he best fit to the surface displacement for the 1976 earthquakes is ob tained from the geometries that are derived from the homogeneous stres s tensor inversion. The inversion of vertical surface displacements fo r the 1984 event constrains the associated fault plane to correspond t o a NE-WS striking and SE dipping plane. The inversions of complementa ry geophysical data argue for the complexity of the orientations of th e faults activated by the 1976-1984 seismic sequence. The 1984 earthqu ake fault plane is well orientated to allow failure to be activated by an horizontal sigma(1) under a Mohr-Coulomb failure criterion. Under the same failure criterion and stress conditions, unlike the 1984 frac ture plane, the 1976 fault planes are misorientated and likely to corr espond to preexisting discontinuities. Concerning the principle stress orientations, the Gazli region seems to be under control of the regio nal tectonic setting. From a regional point of view, the WNW-ESE strik e of sigma(1) and the NNE-SSW strike of sigma(2) deduced from this stu dy for the Kyzylkum Desert can be explained at once by the interaction of the regional plate boundary motions.