Browsing ELibrary by Author "Zagornaya N.Yu."
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- Browsing ELibrary by Author
JavaScript is disabled for your browser. Some features of this site may not work without it.
Browsing ELibrary by Author "Zagornaya N.Yu."
Now showing items 1-10 of 10
-
Anisimova I.V.; Kotov A.B.; Glebovitsky V.A.; Sal'nikova E.B.; Yakovleva S.Z.; Velikoslavinsky S.D.; Zagornaya N.Yu. (2006)The available geological, geochronological, geochemical, and isotopic data furnish evidence that the Paleoproterozoic protoliths of metavolcanic rocks in the central Aldan Shield were formed within a geodynamic system of ...
-
Kovach V.P.; Kotov A.B.; Sal'nikova E.B.; Velikoslavinskii S.D.; Zagornaya N.Yu.; Berezkin V.I.; Smelov A.P. (1999)First investigation results on Sm-Nd isotope systems in clastic metasedimentary and metavolcanic rocks from the high-grade metamorphic supracrustal complexes of central Aldan Shield are used to approximately evaluate their ...
-
Kotov A.B.; Anisimova I.V.; Glebovitsky V.A.; Kovach V.P.; Sal'nikova E.B.; Zagornaya N.Yu.; Smelov A.P.; Berezkin V.I. (2004)The main features in the geological structure of the western Aldan Shield are largely determined by nearly meridional and NE-trending fault zones that host numerous tectonic fragments composed of weakly metamorphosed ...
-
Kozakov I.K.; Kovach V.P.; Kotov A.B.; Salnikova E.B.; Zagornaya N.Yu.; Yarmolyuk V.V. (2003)The compositions of igneous rocks from the Tuva-Mongolia massif were studied. These rocks were formed during the precollisional, syncollisional, and postcollisional stages of massif formation. The compositions of strongly ...
-
Velikoslavinsky S.D.; Kotov A.B.; Sal'nikova E.B.; Kovach V.P.; Glebovitsky V.A.; Zagornaya N.Yu.; Yakovleva S.Z.; Anisimova I.V.; Fedoseenko A.M.; Tolmacheva E.V. (2006)Geochemical data indicate that the protoliths of the overwhelming majority of the metamorphic rocks composing the Fedorov Complex in the Aldan granulite megacomplex were volcanic rocks of three groups, which occur in ...
-
Kovach V.P.; Kotov A.B.; Salnikova E.B.; Zagornaya N.Yu.; Berezkin V.I.; Smelov A.P. (1996)The first data on the Nd isotopic composition in high-AI gneisses and associated gamet-hypersthene-biotite plagiogneisses of the Kurumkan Subgroup, the lengra Group of Aldan Shield are presented. The obtained results show ...
-
Podkovyrov V.N.; Kotov A.B.; Larin A.M.; Kotova L.N.; Kovach V.P.; Zagornaya N.Yu. (2006)The Early Proterozoic was characterized by the development of large epicratonic depressions, which often host large and unique deposits of Cu, Pb, Zn, U, Au, Fe, phosphorites, barite, fluorite, and other mineral resources. ...
-
Myskova T.A.; Glebovitskii V.A.; Miller Yu.V.; L'vov A.B.; Kotov A.B.; Kovach V.P.; Zagornaya N.Yu. (2003)Two section types are established in the Chupa nappe of the Early Precambrian Belomorian mobile belt (BMB) of the Baltic shield: one in the Lake Verkhnee Pulongskoe area of the stratotype region (Chupa Complex) and the ...
-
Velikoslavinsky S.D.; Kotov A.B.; Sal'nikova E.B.; Glebovitsky V.A.; Kovach V.P.; Zagornaya N.Yu.; Belyaevsky N.A.; Yakovleva S.Z.; Fedoseenko A.M. (2003)The results of geochronological investigation confirm the assumption of the Early Proterozoic age of Fedorov rock mass. The estimated age (2006±3 mln years) of metaandesite protolytes of this series agrees with age estimates ...
-
Salnikova E.B.; Kotov A.B.; Belyatskii B.V.; Yakovleva S.Z.; Morozova I.M.; Berezhnaya N.G.; Zagornaya N.Yu. (1997)U-Pb dating of zircons from the reference granitoid complexes showed that principal thrusts in the northern flank of the junction zone between the Olekma granite-greenstone and Aldan granulite-gneiss terranes of the Aldan ...
Now showing items 1-10 of 10
Search DSpace
Browse
-
All of DSpace
-
This Collection