V dannoy rabote obosnovyvaetsya sushchestvovanie edinogo volnovogo mekhanizma, pod vozdeystviem kotorogo, proiskhodit formirovanie tektonicheskikh struktur i migratsiya veshchestva planety. Odnovremennoe proyavlenie na poverkhnosti materikov razlichnoy stepeni intensivnosti endogennykh rezhimov, daet vozmozhnost' shirokogo primeneniya metoda analogii v geologii. Bez dannykh tochnykh nauk, na kotorykh baziruyutsya mnogie otrasli geologicheskogo znaniya, nevozmozhno poznat' sut' geologicheskikh protsessov i sozdat' obshchuyu teoriyu Zemli. Geologiya imeet svoi, prisushchie tol'ko ey zakony, kotorye svyazyvayut mezhdu soboy zakony fiziki i khimii, proyavlyayushchiesya v techenie dlitel'nogo otrezka vremeni. Vse fiziko-khimicheskie protsessy, proiskhodyashchie v geologicheskom prostranstve sistemy Zemli, rassmatrivayutsya vo vzaimosvyazi i vo vzaimozavisimosti. Dannaya 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.