The Study of the Permeability of the Upper Crust Part on the Photo Image of the Surface in the Area of the Nalychevo Field of Thermomineral Waters (Kamchatka)

The study of tectonic break of the upper layer of the earth's crust in the area of the Nalychevo field of thermomineral waters was made. The source material was the results of decryption of aerial-and space images. The specific length of the lineaments (SLL) of the supposed faults was determined up to the depth of 3 km and a 3D matrix was created. The voxel image of the SLL of the investigated block with areas of increased crust permeability was constructed. The Nalychevo field is located at the intersection of the north-western, latitudinal and submeridional zones of increased permeability, which are distinguished in the voxel model by the maximum values of the SLL.