Mekhanizm Formirovaniya Struktury Sistemy Zemli

Sistema tektonosfery porozhdaet vremennye i prostranstvennye neodnorodnosti tektonicheskikh dvizheniy, stol' vazhnye dlya geologov s teoreticheskoy i prakticheskoy tochki zreniya, a takzhe fiziko-khimicheskie protsessy, geneticheski svyazannye s silami gravitatsii i s tsentrobezhnoy siloy vrashchayushcheysya sistemy Zemli. S zonami intensivnoy stepeni pronitsaemosti (deformatsii), svyazyvaetsya formirovanie krupnykh i gigantskikh mestorozhdeniy poleznykh iskopaemykh. V dannoy rabote obosnovyvaetsya sushchestvovanie edinogo mekhanizma, pod vozdeystviem kotorogo, proiskhodit formirovanie tektonicheskikh struktur i migratsiya veshchestva planety. V roli glavnogo deystvuyushchego faktora rassmatrivayutsya deformatsii - kak generatory energeticheskoy volny. Rabota rasschitana ne tol'ko na spetsialistov-geologov, no i na shirokiy krug estestvoispytateley. V rabote v polnoy mere osvyashchen vopros formirovaniya sistemy Zemli, gornykh sooruzheniy, okeanicheskikh vpadin, mestorozhdeniy i rudnykh tel.