Выпуск: 5 , Том: 13 , Год издания: 1972

Deep fault zones are discussed as "bed-like" steep lying bodies of sedimentary Earth Mantle separated by structural and compositional indications. Among them are longitudinal intregeosynclinal and transectional deep fault zones in addition to marginal sutures. Deep fault zones are frequently adjacent to the groupped belts; by the type of intrusive rocks the belts are subdivided into "gabbroid-hyperbasitic" (Penzhin-Pekulnei, Kamchatka-Vyvensky, etc.) and "granitoidal" (Kolyma-Indigirka, East Asia). The belts of the transectional deep fault zones are frequently "amagmatic"