ON the fluid zonality of the consolidated Earth's crust according to cdpm-dss acquisition. Part 1. The continental crust (gas distribution)
The article discusses the results of seismic observations of CDPM and DSS, performed in areas with different geologic structures Vertical and horizontal regions zones with different phase composition of the fluid are distinguished revealed. The physical rational explanation for horizontal zonality of the consolidated Earth's crust is determined not only by the rheological lamination, but also by the phase composition of a fluid. The fluid zonality in fractures has been highlighted as follows. The upper part of the consolidated crust is characterized by a predominantly gas composition, and the middle and lower crust has a saturated composition.