Geologicheskii Vestnik

Location of work: Institute of Geology — Subdivision of the Ufa Federal Research Centre of the Russian Academy of Sciences (IG UFRC RAS) (Ufa, Russia)

E-mail: MinikeevaLR@bashneft.ru

Author's articles

• Possible “current climate images” of deposits of various lithostratigraphic units of the Ural’s Riphean and Vendian
• Clayey rocks of the Upper Proterozoic Suirovo Formation, western slope of the Southern Urals: the main features of lithochemistry
• Terrigenous rocks, discriminant diagrams and paleogeodynamics
• Clayey rocks of the Upper Proterozoic suirovo formation, western slope of the Southern Urals: some features of geochemistry
• Vendian in explanatory notes to sheets of state geolkarta-1000 / 3 N-40 — Ufa And O-40 — Perm: questions of an amateur
• Composition of provenances for the Vendian Kukkarauk Formation of the Southern Urals (comparison of petrographic and lithochemical data)
• Trends in changes in a number of geochemical parameters of the composition of fine-grained clastic rocks of the Lower Riphean sedimentary sequences of the northeastern and central parts of th
• Yurmatinian/Karatavian boundary in the Riphean stratotype: comparison of the geochemical features of clay rocks of Avzyan Formation and Biryan Subformation of Zilmerdak Formation
• Diagrams with composition fields of the pelitic fraction of bottom sediments in the estuarine parts of different modern river’s categories: another approach to verification
• Fine-grained clastic rocks of shelf and turbidite sedimentary associations: position of data points on various discriminant diagrams
• Position of data points of the riphean stratotype clay rocks on the diagrams for the provenance
• Detrital zircon. Some aspects of the problem (brief overview of the ideas)
• Comparison of geochemical characteristics of clastic rocks of different grain size classes based on the example of jurassic deposits of the North-Pokachevskoye oil field (Shirotnoye
• FeT/Al values in Upper Precambrian clay rocks of the Volga-Ural region and the redox-status of Meso-Neoproterozoic ocean waters