Results 131 to 140 of about 2,204,508 (267)
Rock flows are defined as forms of spontaneous mass movements, commonly found in mountainous countries, which have been studied very little. The article considers formations known as rock rivers, rock flows, boulder flows, boulder stria, gravel flows ...
Matveyev, S. N.
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Identification of USSR Indicator Regions [PDF]
Potential indicator regions were determined by comparing the statistics for barley and wheat at the lowest administrative levels for which published statistics were available.
Breigh, H., Disler, J.
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Dataset of diatom abundances and diatom-inferred total phosphorus and electrical conductivity for Lake Tavatui (Middle Urals, Russi) over the last 11.7 cal ka BP. [PDF]
Maslennikova AV.
europepmc +1 more source
Institutional Transition and Local Self-Government in Russia [PDF]
This paper includes the following parts: 1) "Vertical or Triangle? Local, regional and federal government in the Russian Federation after Law 131.", by Adrian Campbell, and 2) comments to the paper "Softness and hardness of the institutions in Russian ...
Adrian Campbell +3 more
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Analysis of the Potential Range of Anticlea sibirica L. (Kunth) and Its Changes under Moderate Climate Change in the 21st Century. [PDF]
Fedorov N +5 more
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Geochemical features of groundwater in the South Urals
This paper gives an analysis and generalization of the data on groundwater chemical and gas composition, located deep in the largest tectonic structures of the Urals. The distribution of groundwaters by the degree of mineralization and composition is subjected to the normal vertical hydrogeochemical zonation.
R. F. Abdrahmanov, V. G. Popov
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TITANITE OF THE VISHNEVOGORSKY ALKALINE COMPLEX (South Ural)
Titanite CaTi(SiO4 )O is a common accessory mineral of alkaline rocks and pegmatites of the Vishnevogorsky alkaline complex, South Urals. It occurs in many magmatic assemblages, is found in some metasomatites, underwent deformation and recrystallization.
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ALUMOENSTATITE FROM KARABASH AND NYASHEVO MASSIFS (SOUTH URAL)
Aluminoenstatite was found in the rocks of the Karabash and Nyashevo massifs (South Urals). The features of its chemical composition (high Al contents), along with textural-structural peculiarities of the rocks, indicate a range of its formation conditions. The high Al2 O3 contents (15.3– 20.0 wt. %), elevated Fe contents, and noticeable Na contents in
E.V. Medvedeva +3 more
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