Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Yu. N. Yakovlev"'
Publikováno v:
Doklady Earth Sciences. 440:1449-1454
The basement of the Paleoproterozoic Pechenga structure was cored by the Kola superdeep borehole SD-3 at the depths of 6842–12 262 m. It consists mainly of alternating strata of metavolcanic daciteplagiorhyodacite rocks and high-alumina gneisses; t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a7c253869a457817edf28dcbd7e87feb
https://doi.org/10.1134/s1028334x11100266
https://doi.org/10.1134/s1028334x11100266
Autor:
D. M. Guberman, Yu. N. Yakovlev, V. A. Muhamedov, V. S. Lavrov, A. V. Nikolaev, A. S. Belyakov, Alexey Lyubushin, A. D. Zhigalin
Publikováno v:
Doklady Earth Sciences. 412:97-100
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1d5eeee71cb5ed7419a9f08b51173542
https://doi.org/10.1134/s1028334x07010229
https://doi.org/10.1134/s1028334x07010229
Autor:
O. G. Chernova, A. K. Yakovleva, M. S. Babushkina, Simon A. T. Redfern, Yu. N. Yakovlev, N. O. Ovchinnikov, L. P. Nikitina
Publikováno v:
Mineralogical Magazine. 66:491-512
Trioctahedral ferromagnesium micas from the Archaean amphibolites of the Kola super-deep borehole (KSDB-3) complex have been compared with those from analogous Archaean surface rocks in an integrated study of their chemical compositions and structura
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a3a23baed35360f18118ae683457c88a
https://doi.org/10.1180/0026461026640044
https://doi.org/10.1180/0026461026640044
Publikováno v:
Journal of Engineering Physics and Thermophysics. 63:943-948
A mathematical model of hydrodynamics is proposed for filling closed volumes with allowance for air capture by a liquid jet. Adequacy of the model is established by comparison between the calculated and experimental data obtained by means of physical
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f926a5ffad94af906abf6df9cfc84cf4
https://doi.org/10.1007/bf00852785
https://doi.org/10.1007/bf00852785
Autor:
S. A. Razhev, F. P. Mitrofanov, Yu. N. Yakovlev, Tatiana L. Grokhovskaya, N. N. Veselovsky, V. V. Distler
Publikováno v:
Mineralogy and Petrology. 43:181-192
During the last few years nearly 50 minerals and unnamed platinum-group element (PGE) phases have been identified by the authors in nickel-bearing mafic-ultramafic massifs of the Kola region. About 20 established PGE minerals have been found whilst m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55b967cbe4ed486878ab0536d7f1284d
https://doi.org/10.1007/bf01166890
https://doi.org/10.1007/bf01166890
Autor:
Yu. N. Yakovlev, M. S. Rusanov, A. K. Yakovleva, Yu. P. Smirnov, V. S. Lanev, S. V. Ikorsky, Igor Tolstikhin, V. R. Vetrin, F. P. Mitrofanov, Yu. N. Neradovsky
Publikováno v:
Super-Deep Continental Drilling and Deep Geophysical Sounding ISBN: 9783642501456
A considerable amount of new information about the features of rocks and ore formation at various depths has been obtained due to the investigations carried out by the Geological Institute of the Kola Science Centre, USSR Academy of Sciences, and the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fca08f286dbac688bb93f11574cd840a
https://doi.org/10.1007/978-3-642-50143-2_34
https://doi.org/10.1007/978-3-642-50143-2_34
Publikováno v:
International Geology Review. 13:1062-1068
The mineralized area (fig. 1) lies inside a large dunitic body. The sulfides are small phenocrysts of pentlandite (with chalcopyrite and pyrrhotite); chromite is generally present and metasomatic magnetite is locally abundant, as replacer of the sulf
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e246e0444fb4f3a7cf5c054b2cfe86df
https://doi.org/10.1080/00206817109475537
https://doi.org/10.1080/00206817109475537
On the Role of Metamorphism in the Formation of Nickel-Copper Sulfide Deposits in the Kola Peninsula
Autor:
A. K. Yakovleva, Yu. N. Yakovlev
Publikováno v:
Special Publication No. 4 of the Society for Geology Applied to Mineral Deposits ISBN: 9783642709043
Three stages are apparent in the formation of the nickel-copper sulfide deposits, viz. magmatic, regional metamorphic, and late metamorphic. In the magmatic stage, syngenetic ores are simple and constant in the composition formed. In the regional met
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f6f4ed02e4d465f8be4ec4a75734fd8
https://doi.org/10.1007/978-3-642-70902-9_9
https://doi.org/10.1007/978-3-642-70902-9_9
Autor:
Yu. N. Yakovlev, V. D. Medvedev, N. F. Potemkin, A. V. Fafinov, Yu. N. Sokolov, V. B. Romashevskii
Publikováno v:
Chemical and Petroleum Engineering. 17:550-551
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5592bf8405260c14170faede112eb7f0
https://doi.org/10.1007/bf01155014
https://doi.org/10.1007/bf01155014