“Living” granites and intragranite hydrocarbon deposits

There is a question: what is the reason for the "aliveness" of already hardened granite masses, their extraordinary mobility and ability to penetrate the earth’s crust, what is the mechanism of their loosening, granulation and structural transformations? These aspects of "granite geology" can be considered from the point of view of a structural-tectonic model of the formation of hydrocarbon deposits within granite massifs.