Redox zonality of the Sikhote-Alin organic belt, connection with geodynamics

The study of the redox conditions of crystallization of igneous rocks zoning in the Sikhote-Alin orogenic belt has allowed the authors to make a conclusion: there is a redox background in the lithosphere of the region where all magmatic activity occurs. The background does no. depend on the age and petrographic features of igneous rocks. It depends on the position of oceanic and continental plates in convergent zones.