Recent Hydrodynamic Activity of Submeridional Deep-Seated Fault Zones As an Indicator of the Petroleum Resource Potential of Sedimentary Basins (Northeastern Russia)

摘要

The defined submeridional deep-seated fault zones (SDFZ) may be considered as global geological structures comparable with rifts [ 11. The rifts border usually separate lithospheric blocks or plates determining their configurations. The submeridional deep-seated fault zones, which also represent superposed structures, leave the contours of host geological objects unchanged. They are formed by closely spaced submeridional deep-seated subvertical faults approximately 100—150 km wide and thousands of kilometers long.