Про шляхи втілення глибинного високотемпературного флюїду в земну кору

Abstract

Two ways of a realization of the intrusion process of a deep-seated high-temperature fluid in the Earth crust are substantiated. It is shown that the synthesis of hydrocarbons and minerals in the deep-seated high-temperature fluid medium is possible only in the case where the stratum of overlying rocks in a definite area of the Earth crust can stand the considerable fluid pressure and temperature. Otherwise, the relief of the fluid into the Earth surface occurs.