Zobrazeno 1 - 10
of 10
pro vyhledávání: '"I.A. SHVAIKA"'
Publikováno v:
Mineralogical Journal. 44:73-83
The Middle-Dnieper megablock, which is a fragment of the craton, differs from other cratons found on Earth. This is because of the large variety of granitoids (Tokiv, Mokro-Moskowka, and Demuryne complexes) in the former that were formed after the Me
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0ed93d9e738225ea21315726797faa84
https://doi.org/10.15407/mineraljournal.44.04.073
https://doi.org/10.15407/mineraljournal.44.04.073
Publikováno v:
Mineralogical Journal. 44:48-66
Trace element concentrations (REEs, Y, Sr, Th, U) in apatites from the most typical rocks of the Korsun-Novomyrhorod anorthosite-rapakivi pluton (KNP) were measured. Apatite was the last liquidous phase to crystallize in all the studied rocks because
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3bac8b1b557491423f1f3a14a038169e
https://doi.org/10.15407/mineraljournal.44.03.048
https://doi.org/10.15407/mineraljournal.44.03.048
Publikováno v:
Mineralogical Journal. 44:20-47
The geochemical features of most distributed rocks from the Korsun'-Novomyrhorod Pluton are considered. The obtained data give reason to assume that the association of basic and intermediate rocks of the pluton was formed because of the differentiati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::34b2de385422b829ed1a1dcf6322538c
https://doi.org/10.15407/mineraljournal.44.01.020
https://doi.org/10.15407/mineraljournal.44.01.020
Autor:
G.V. ARTEMENKO, L.M. STEPANYUK, I.A. SAMBORSKA, B.V. BORODYNYA, I.A. SHVAIKA, K.I. GOGOLEV, L.I. PROSKURKA
Publikováno v:
Mineralogical Journal. 43:63-72
In the Saltych anticlinorium of the West Azov, small intrusions of rocks of basic and ultrabasic composition are known in the middle reaches of the Obitochna, Kiltychiya and Burtychiya rivers and in the upper reaches of the Obitochna river. They are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e85c6038eba2ffd4d6be4cb756ffda7b
https://doi.org/10.15407/mineraljournal.43.04.063
https://doi.org/10.15407/mineraljournal.43.04.063
Features of REE Distribution in Apatites of Granulite-Gneiss Rocks of Podilsk Block Ukrainian Shield
Autor:
L.I. Proskurka, I.M. Lisna, O.M. Ponomarenko, I.D. Shvaika, Anatolyi Samchuk, I.A. Shvaika, L.V. Somka, K.V. Vovk
Publikováno v:
Mineralogical journal. 42:27-38
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::15179e5d16b18eab62ac87fd31a5f8c9
https://doi.org/10.15407/mineraljournal.42.03.027
https://doi.org/10.15407/mineraljournal.42.03.027
Publikováno v:
Мінеральні ресурси України, Iss 4, Pp 3-8 (2019)
Fluorite is one of the main concentrators of rare earth elements (REE) in the granites of the Ruska Polіana massif of the Korsun-Novomyrhorod pluton of the Ukrainian Shield. Despite its distribution in the granites of the massif, the geochemical fea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d3ced3e162b29c1cddeff12934df22ad
https://mru-journal.com.ua/index.php/mru/article/view/43
https://mru-journal.com.ua/index.php/mru/article/view/43
Publikováno v:
Geological Journal. :91-102
The late paleoarhean (3297±22 Ma) age of tonalite gneisses was at first identified on West-Azov block. They are characterized by a positive value of eNd(3300) = 0,3÷1,8, that they are juvenile source. With the new geochronological data, in the west
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cb2cc18beedc9639e3c8096eb3394ec2
https://doi.org/10.30836/igs.1025-6814.2014.4.139191
https://doi.org/10.30836/igs.1025-6814.2014.4.139191
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