RELATIONS BETWEEN CRUSTAL BLOCKS AND EVOLUTION OF THE SAN ANDREAS FAULT SYSTEM
Balanced reconstruction of basement rocks and overlying strata along the SAF system reveals the pre-late Cz paleogeology of southern CA (Powell, 1993). Palinspastically restored assemblages define three major basement blocks: the Peninsular Ranges and Sierra Nevada batholiths (PRB & SNB) and an intervening block formed by reassembly of crystalline rocks of the Mojave Desert-Transverse Ranges-Salinian proto-block (MTSB) (Powell, 1981).
As transform-margin deformation evolved, the PRB and SNB acted as rigid blocks between deforming crust to the E and W (Great Basin/Walker Lane E of SNB and Coast Ranges/SAF W of SNB; Sonoran Basin and Range/Gulf of CA E of PRB and continental borderland W of PRB). In contrast, faults were distributed through the MTSB, which was deformed sequentially by zones of transtensional dextral shear, by sets of right- and left-lateral faults, and ultimately by contractional folding and thrusting. As do the SNB and PRB, the MTSB consists of Mz batholithic rocks--but in contrast to those blocks, the MTSB also contains widespread exposures of Proterozoic crust and is underplated by Mz oceanic crust and metamorphosed Mz-Cz rocks in exposures of Pelona-Orocopia-Rand Schist exhumed beneath low-angle faults.
The evolving strain pattern suggests that the rigid PRB and SNB rotated clockwise within right-lateral couples, whereas the more pervasively deforming crust of the MTSB, bounded to the N by the evolving Garlock Fault and to the S by faults along the S flank of the Transverse Ranges, responded as a more readily deformable “soft” domain in a sinistral couple between the two rigid blocks. As plate-margin deformation progressed the PRB and SNB indenters converged on one another while the MTSB “escaped” from between the two.