Comprehensive Geological and Geochemical Analysis of Sediments of the Sargaev Horizon of the Udmurt Republic

Abstract

The analysis of the bitumoids of the Sargaevskiy horizon of the Middle Frasnian sub-stage of the Upper Devonian is presented. The origin of the rocks is associated with the accumulation of sediments in a relatively deep sea basin, in a reducing and sharply reducing environment. For the purpose of genetic analysis, a geochemical interpretation has been carried out. Numerous traces of the movement of free bitumoids indicate migration-accumulation transformations.

Keywords

• саргаевский горизонт
• доманикиты
• органическое вещество
• битумоиды
• удмуртская республика