PRESSURE CHANGES IN PERMAFROST WATERS

It is noted the need to study the features of the oil and gas content of the upper part of the section in the area of influence of perennial weathered rocks (MMP). The geological description and conceptual model of formation of the Upper Chimidikaen oil phenomenon in the zone of influence of perennial German rocks are given. The characteristic of interpermafrost groundwater type of the Bestyakh terrace r. Lena is given. On the basis of literary data and in situ observations, a mechanism for changing the pressure of inter-permafrost waters is proposed. It is concluded that the presence of oily formations in the frozen zone indicates the proximity of the oil source in the lower part of the cut.