Zobrazeno 1 - 10
of 11
pro vyhledávání: '"E. E. Savchenko"'
Autor:
S. V. Krivovichev, V. N. Yakovenchuk, T. L. Panikorovskii, E. E. Savchenko, Ya. A. Pakhomovsky, Yu. A. Mikhailova, E. A. Selivanova, G. I. Kadyrova, G. Yu. Ivanyuk
Publikováno v:
Доклады Академии наук. 488:526-529
Nikmelnikovite, Ca12Fe2+Fe3+3Al3(SiO4)6(OH)20, is a new mineral from the Kovdor massif, Kola peninsula, Russian Federation. It is the first trigonal member of the garnet supergroup. The mineral is named in honor of Academician Nikolay Nikolaevich Mel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4adb6ac0d9a395b29a262f26fc5efa4b
https://doi.org/10.31857/s0869-56524885526-529
https://doi.org/10.31857/s0869-56524885526-529
Autor:
E. E. Savchenko, Sergey V. Krivovichev, Ya. A. Pakhomovsky, Ekaterina A. Selivanova, Viktor N. Yakovenchuk, Taras L. Panikorovskii, Yu. A. Mikhailova, G. I. Kadyrova, G. Yu. Ivanyuk
Publikováno v:
Doklady Earth Sciences. 488:1200-1202
Nikmelnikovite, Ca12Fe2+Fe$$_{3}^{{3 + }}$$Al3(SiO4)6(OH)20, a new mineral from the Kovdor massif (Kola Peninsula, Russia), is described. It is the first trigonal representative of the garnet supergroup. The mineral is named in honor of Academician N
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e50e6f329531612e56b29005842b41eb
https://doi.org/10.1134/s1028334x19100143
https://doi.org/10.1134/s1028334x19100143
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 539:012151
The low-sulfide palladium deposit North Kamennik is confined to the North platinum-bearing reef in the West Pana intrusion of the Paleoproterozoic Fedorova-Pana layered complex of the Kola Peninsula. The main ore body of this deposit is accompanied b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4bbe74cc890a5f333f6f935d025d0edd
https://doi.org/10.1088/1755-1315/539/1/012151
https://doi.org/10.1088/1755-1315/539/1/012151
Publikováno v:
Geology of Ore Deposits. 53:735-744
Secondary textures formed in natural zircon crystals under the influence of hydrothermal solutions are interpreted as products of metasomatic substitution. Such textures are clearly seen in metamict zircons and zircons enriched in radioactive element
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53167c61fc927d782cb9b7e466ba1fef
https://doi.org/10.1134/s1075701511080071
https://doi.org/10.1134/s1075701511080071
Publikováno v:
Geology of Ore Deposits. 52:843-851
Unusual ultrapotassic dikes were recently found on the Kvaloya Island in Northern Norway. The dikes crosscutting granites 1.8 Ga in age are 0.1–1.0 m thick and consist of phlogopite phenocrysts in a fine-grained groundmass of K-magnesioarfvedsonite
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dd150ea028b824f4ffa0886822ce8782
https://doi.org/10.1134/s1075701510080167
https://doi.org/10.1134/s1075701510080167
Publikováno v:
Geochemistry International. 48:871-890
Zircon from the eclogite-like rocks of the Shirokaya and Uzkaya Salma area (Kola Peninsula) was studied using a complex of mineralogical and geochemical methods (CL, BSE, microprobe, and REE distribution). Different zones distinguished within zircon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1531f1c31af7c0b29e794522c3b153c0
https://doi.org/10.1134/s001670291009003x
https://doi.org/10.1134/s001670291009003x
Publikováno v:
Doklady Earth Sciences. 430:120-124
120 Zircon is characterized by striking typomorphic features (morphology, anatomy, chemical composi� tion), which allow the reconstruction of conditions and stages of its crystallization in different geological processes (magmatic, postmagmatic, an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8582a4572e0d05ac931ab89bb92a87a0
https://doi.org/10.1134/s1028334x10010265
https://doi.org/10.1134/s1028334x10010265
Autor:
Yu. N. Neradovsky, E. E. Savchenko
Publikováno v:
Geology of Ore Deposits. 50:746-748
The Sopcheozero chromite deposit is hosted in dunite of the Monchegorsk layered intrusion as a sheetlike body of disseminated ore with a chromite grade varying from 20 to 60%. The total PGM content in the ore attains 0.5–0.8 g/t. The composition of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f6d10a7af25f5c6cf8291d09076c18c8
https://doi.org/10.1134/s1075701508080102
https://doi.org/10.1134/s1075701508080102
Autor:
Savchenko E; Centro de Estudios Parasitológicos y de Vectores (CONICET-UNLP). Bv. 120 s/n e/ 60 y 64, 1900 La Plata, Argentina., Lareschi M; Centro de Estudios Parasitológicos y de Vectores (CONICET-UNLP). Bv. 120 s/n e/ 60 y 64, 1900 La Plata, Argentina. Electronic address: mlareschi@cepave.edu.ar.
Publikováno v:
Acta tropica [Acta Trop] 2019 Nov; Vol. 199, pp. 105146. Date of Electronic Publication: 2019 Aug 15.
Autor:
Piekkola S; Food and Health Research Centre, Department of Clinical Nutrition, Institute of Public Health and Clinical Nutrition, University of Eastern Finland, PO Box 1627, FI-70211 Kuopio, Finland., Turner PC, Abdel-Hamid M, Ezzat S, El-Daly M, El-Kafrawy S, Savchenko E, Poussa T, Woo JC, Mykkänen H, El-Nezami H
Publikováno v:
Food additives & contaminants. Part A, Chemistry, analysis, control, exposure & risk assessment [Food Addit Contam Part A Chem Anal Control Expo Risk Assess] 2012; Vol. 29 (6), pp. 962-71. Date of Electronic Publication: 2012 Mar 01.