title: Low velocity zones of thermobaric origin in the crystalline crust
abstract: The paper presents a new hypothesis of origin, existence and disappearance of crustal low velocity zones (LVZs), discovered the DSS method as elastic anomalies of the Earth’s crust. Complex changes are experimentally obtained for VР,S=f(PT) in rocks (regions of velocity inversion are revealed). There is cataclastic decompaction of mineral medium in them — dilatancy phenomenon. Their configuration, location and thermodynamic conditions coincide well with the DSS elastic anomalies. They arise only
journal: Geofizicheskiy Zhurnal