Zobrazeno 1 - 7
of 7
pro vyhledávání: '"V. I. Levitsky"'
Publikováno v:
Геодинамика и тектонофизика, Vol 8, Iss 3, Pp 477-480 (2017)
The Siberian craton consists of Archean blocks, which were welded up into the same large unit by ca 1.9 Ga [Gladkochub et al., 2006; Rojas-Agramonte et al., 2011]. The history of the constituent Archean blocks is mosaic because of limited number of o
Externí odkaz:
https://doaj.org/article/07ec2372a35345e6b1fa6834f28becf1
Publikováno v:
Mineralogical Magazine. 81:383-402
Sulfhydrylbystrite, Na5K2Ca(Al6Si6O24)(S5)(SH), cell parameters a = 12.9567(6) Å, c = 10.7711(5) Å, space group P31c, is a new mineral belonging to the cancrinite group. It was found at Malaya Bystraya lazurite deposit, Lake Baikal area, Eastern Si
Publikováno v:
Geodinamika i Tektonofizika, Vol 8, Iss 3, Pp 477-480 (2017)
The Siberian craton consists of Archean blocks, which were welded up into the same large unit by ca 1.9 Ga [Gladkochub et al., 2006; Rojas-Agramonte et al., 2011]. The history of the constituent Archean blocks is mosaic because of limited number of o
Autor:
V. I. Levitsky, L. A. Ivanova, A. N. Sapozhnikov, D. I. Cherepanov, E. V. Kaneva, L. F. Suvorova, L. Z. Reznitsky
Publikováno v:
Geology of Ore Deposits. 54:557-564
The results of an examination of vladimirivanovite, a new mineral of the sodalite group, found at the Tultui deposit in the Baikal region are discussed. The mineral occurs in the form of outer rims (0.01–3 mm thick) of lazurite, elongated segregati
Publikováno v:
Geology of Ore Deposits. 53:678-682
A lazurite sample taken from the Tultui deposits in the Baikal region has been studied using petrographic examination, X-ray diffraction, and local X-ray spectroscopy (electron microprobe). It is established that the line of the basic cell in the X-r
Autor:
A. M. Mazukabzov, S. Z. Yakovleva, Eugene V. Sklyarov, V.S. Fedorovsky, A. V. Lavrenchuk, A. E. Starikova, I. V. Anisimova, A. B. Kotov, V. I. Levitsky, A. M. Fedoseenko, E. B. Sal’nikova
Publikováno v:
Russian Geology and Geophysics. 50:1091-1106
Carbonatites associated with syenites and subalkalic mafic rocks (lamprophyres) occur in the Himalayan continental collision zone, and this suggests their possible existence in other Phanerozoic collisional settings. The Early Paleozoic Ol’khon col
Publikováno v:
Lithology and Mineral Resources. 39:230-242
Complete geochemical characteristics have been found for calcareous–silicate rocks of the Kharagol Formation that serves as a reference unit within the Khamardaban polymetamorphic composite terrain (southern folded framing of the Siberian Platform,