Monographs

Synrift sedimented associations (a number of lythochemical scetches)Maslov A.V., Podkovirov V.N.

Year: 
2020

To interpret the paleogeodynamic settings of the formation of terrigenous strata since the early 1980s. data on the bulk chemical composition of sandstones and fine-grained clastic/clay formations

Precambrian complexes of the Isherim anticlinorium (Northern Urals):stratigraphy, magmatism, metamorphism, metallogeny

Year: 
2020

The book is devoted to the characteristics of the Precambrian complexes of the Isherim (Vishera-Kutim) anticlinorium located in the axial part of the Northern Urals. New data on stratigraphy, magmatism, metamorphism and metallogeny are presented, including those obtained using new geochemical, isotope-geochronological methods and predictive mineralogical studies.

Granite pegmatites and pegmatoids of the Urals. Ogorodnikov V.N.,Polenov Yu.A., Kisin A.Yu. Savichev A.M.

Year: 
2020

Despite significant progress in the study of pegmatites, the reasons for the empirically established dependence of their type on the features of the geological structure and evolution of those structural-formational zones in which they form have not yet been studied.

Folded basement of the Yamal peninsula and its constructive bounds. K.S. Ivanov, Yu. V. Erokhin, V. N. Puchkov. V. S. Ponomarev, N.P. Kostrov, V.V. Khiler

Year: 
2021

 The book is devoted to one of the most poorly studied issues of the geology of the West Siberian megabasin - namely, the geology of the basement of the Yamal Peninsula. The peninsula contains huge reserves of hydrocarbon raw materials, and therefore an attempt to generalize all the available information about the geology of its basement is justified and relevant.

"Algoflora and microfacies of the Lower Carboniferous of the Urals and adjacent territories" R.M. Ivanova, T.I. Stepanova

Year: 
2021

The results of the study of algoflora and microfacies from the Lower Carboniferous deposits developed in the Middle and Southern Urals, as well as on the territory of the western slope of the Northern Urals, Novaya Zemlya and the Tyumen-Kustanai trough are presented. The composition of algal associations in the stratigraphic interval from the Kizelovsky horizon of the Tournaisian stage to the Serpukhovian stage, inclusive, is considered and analyzed. The dependence of the composition of algoflora complexes on the facies features of sedimentation environments has been established.