Zobrazeno 1 - 10
of 46
pro vyhledávání: '"V. A. Glebovitsky"'
Autor:
I. S. Sedova, V. A. Glebovitsky
Publikováno v:
Geology of Ore Deposits. 60:658-671
The evolution of rock-forming minerals (orthopyroxene, garnet, biotite, and amphibole) is studied in successive generations of granites and leucosomes. It is shown that the trace element partition coefficients between solid phases and melt are govern
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::47801122a3e958f3b03b178790f61ac0
https://doi.org/10.1134/s1075701518080032
https://doi.org/10.1134/s1075701518080032
Publikováno v:
Doklady Earth Sciences. 479:295-299
The P–T conditions of Early Paleozoic metamorphism in the Sangilen block of the Tuvino-Mongolian Massif (southeastern part of the Central Asian Mobile Belt) achieved a value of 910–950°C and 3–4 kbar, which corresponded to the conditions of ul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f40c8031ae1987e750ceee348472f4d3
https://doi.org/10.1134/s1028334x18030145
https://doi.org/10.1134/s1028334x18030145
Autor:
Yu. M. Lebedeva, A. A. Andreev, S. D. Velikoslavinsky, V. A. Glebovitsky, E. V. Tolmacheva, E. S. Bogomolov, E. Yu. Rytsk
Publikováno v:
Doklady Earth Sciences. 479:342-346
The Kichera zone of the Baikal–Muya Belt consists of alternating tectonic plates with rocks of different metamorphic facies. Garnet–cordierite–sillimanite gneiss from the tectonic fragment in granite–gneiss of the Baikal massif with an age of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::10123f0a6471df379f8ff4fe556608be
https://doi.org/10.1134/s1028334x18030054
https://doi.org/10.1134/s1028334x18030054
Autor:
Anton R. Chakhmouradian, V. A. Glebovitsky, M. V. Stifeeva, E. B. Sal’nikova, Ekaterina P. Reguir
Publikováno v:
Doklady Earth Sciences. 478:148-151
The geochronological U–Pb study of shorlomite from igneous rocks of the alkali–ultramafic Afrikanda massif (Kola Peninsula) was performed. The results demonstrate the reliability of calcium garnet as a mineral for the U–Pb geochronology of a wi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f4c949430da6c23854211e3ffa1eaad
https://doi.org/10.1134/s1028334x18020083
https://doi.org/10.1134/s1028334x18020083
Autor:
V. F. Proskurnin, Yu. Yu. Yurchenko, V. N. Zelepugin, E. S. Bogomolov, V. K. Kuz'min, V. A. Glebovitsky, N. V. Rodionov
Publikováno v:
Doklady Earth Sciences. 478:31-35
The first results of U–Pb SIMS geochronological and Nd–Sr isotope–geochemical studies of the Yurovka Complex metavolcanics and granitoids of the Luktur Complex belonging to the Yurovka Swell yielded a Paleoproterozoic age of their formation poi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::811a87dc1a6986b19b675b2e842e97b2
https://doi.org/10.1134/s1028334x18010130
https://doi.org/10.1134/s1028334x18010130
Publikováno v:
Geology of Ore Deposits. 59:687-706
The study of the Lukkulaisvaara layered massif from the Olang group of intrusions in northern Karelia corroborates the important role of supplementary intrusive phases of PGE mineralization. Injection and crystallization of new magma portions result
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c9b39cc4deacf314e227a1c9d6195d60
https://doi.org/10.1134/s1075701517080098
https://doi.org/10.1134/s1075701517080098
Autor:
V. A. Glebovitsky, L. M. Stepanyuk, Yu. S. Egorova, Sergey Sergeev, Sergey G. Skublov, V. V. Balagansky, K. O. Lokhov, S. B. Lobach-Zhuchenko, Sh. K. Baltybaev, O. L. Galankina
Publikováno v:
Doklady Earth Sciences. 477:1391-1395
Complex study of the U–Pb and Lu–Hf systems of zircon from a lhertzolite lens of Archean gneiss enderbites of the Bug complex, Ukrainian Shield, showed that ultramafic magma was contaminated by the material of the country gneiss enderbites. The a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::963b4bdcec2acdb01d769ac0b54b3bb5
https://doi.org/10.1134/s1028334x17120157
https://doi.org/10.1134/s1028334x17120157
Autor:
D. P. Krylov, V. A. Glebovitsky
Publikováno v:
Doklady Earth Sciences. 475:818-821
Based on the density functional theory (DFT), frequency shifts of garnet end-members upon isotope substitutions (18O/16O, as well as “non-traditional” stable isotopes) were calculated. According to the calculations, the temperature dependencies o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f0c13a98b7806aecdc79c1c144961fc3
https://doi.org/10.1134/s1028334x17070236
https://doi.org/10.1134/s1028334x17070236
Autor:
E. B. Sal’nikova, V. A. Glebovitsky, E. Yu. Rytsk, A. M. Fedoseenko, S. D. Velikoslavinsky, I. A. Alekseev, Yu. V. Plotkina
Publikováno v:
Doklady Earth Sciences. 474:569-573
This work presents the results of U–Pb isotope dating of zircons from granodiorites and plagiogranites of the Tallainskii gabbro–granodiorite–plagiogranite complex of the Karalon–Mamakan zone of the Baikal–Muya belt, ascribed to the Tallain
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6496363b5d0203d36230a27c19005a06
https://doi.org/10.1134/s1028334x17050166
https://doi.org/10.1134/s1028334x17050166
Autor:
V. P. Chekulaev, V. A. Glebovitsky
Publikováno v:
Doklady Earth Sciences. 472:78-82
The possibilities of using the average compositions of tonalite–trondhjemite–granodiorite association rocks (TTG), which make up a significant part of the Archaean continental crust, have been examined. The results of the TTG average compositions
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d1d06f28d2b0e7767ea34c70cc938ff1
https://doi.org/10.1134/s1028334x17010135
https://doi.org/10.1134/s1028334x17010135