On geochemical behaviour of fluorine, sulfur, phosphorus and carbon in sedimentary processes

Is indicated that the tendencies of change of contents CO2 and C are well compounded with the data about their distribution in Paleozoic deposits and arid deposits of the Russian platform and western Siberia. At the same time Mesozoic deposits of the Tajik depression are characterized by heightened contents of fluorine in sandstones and in fossil rocks, sulfur and arid sandstones and phosphorus-in sandstones concerning their clark