Year: 2022
Pages: 16-33
UDC: 551.72; 552.3
Number: 3
Type: scientific article
BBK: 63.4 (235.55)
DOI: 10.31084/2619-0087/2022-3-2
Topic: ARTICLES AND PUBLICATIONS
Authors: Michurin, Sergey V., Krupenin, Mikhail T., Shiyanova, Evgeniya O., Saveliev, Dmitry E., Gorozhanin, Valery M., Dub, Semyon A., Kazbulatova, Gulfiya M., Akhmedova, Regina R., Sharipova, Aisylu A.
Тhe results of the study of stratigraphy and conditions of occurrence of rocks of the stratotypic section of the Tulmen sub-formation are considered, and the characteristic of gabbrodolerites breaking through sedimentary rocks is also given. It is shown that the boundaries of the layers in the section are not stratigraphic, but tectonic, representing thrusts or underthrusts, which implies a stratigraphic incompleteness of the section. Gabbrodolerites of the Tulmen section are characterized by relatively low carbonate and magnesia content and high contents of TiO2, P2O5 and the sum of alkalis Na2O+K2O with a predominance of sodium over potassium. They demonstrate above-clarke concentrations of F, Cl, V, Va and below-clarke — Cr, Ni, Sr. According to petro- and geochemical features, they are close to the rocks of the Miselinsky complex of alkaline gabbroids. The obtained results on mineralogy and geochemistry of sedimentary rocks of the Tulmen section suggest that the formation of chlorite, biotite, phlogopite in them and the enrichment of rocks with fluorine by 2–7 times above clarke could be associated with the activity of postmagmatic fluids.
tyulmen sub-formation, Avzyan formation, gabbrodolerites, Miselinsky complex, alkaline gabbroids