Zobrazeno 1 - 10
of 142
pro vyhledávání: '"V. G. Vladimirov"'
Publikováno v:
Геодинамика и тектонофизика, Vol 15, Iss 4 (2024)
The first U-Pb isotope-geochronological data were obtained on the age of early collisional granitoids of the Matut massif (Western Sangilen, SE Tuva). The rocks that have been studied are assigned to magnesian, calc-alkaline, high-potassium, and low-
Externí odkaz:
https://doaj.org/article/095f537f3ff448fb9f9ceaa6670766b1
Publikováno v:
Геодинамика и тектонофизика, Vol 13, Iss 2 (2022)
A critical element in the construction of tectonic models of exhumation of basalts that have undergone high-pressure metamorphism is the diagnosis of synchronicity and the genetic relationship between deformations and high-pressure metamorphic change
Externí odkaz:
https://doaj.org/article/adfd27c423b14e269bd83ea6b045a369
Publikováno v:
Геодинамика и тектонофизика, Vol 10, Iss 2, Pp 325-345 (2019)
This article is focused on the intrusion and formation of combined dykes. Two main groups of conventionally magmatic mingling are distinguished: (1) plutonic bodies, and (2) combined dykes. The first group is represented by small basite inclusions th
Externí odkaz:
https://doaj.org/article/fa0916efc80445278499bf6ef746ac73
Publikováno v:
Геодинамика и тектонофизика, Vol 8, Iss 2, Pp 217-222 (2017)
This issue of Geodynamics & Tectonophysics presents the state-of-the-art studies of mingling processes and investigations of the interactions between the mafic and acidic melts of contrasting compositions at various depths of the Earth's crust. The d
Externí odkaz:
https://doaj.org/article/86b32a5e7ad24d1c9cc4cfee93d045ce
Autor:
O. P. Polyansky, A. N. Semenov, V. G. Vladimirov, I. V. Karmysheva, A. G. Vladimirov, V. A. Yakovlev
Publikováno v:
Геодинамика и тектонофизика, Vol 8, Iss 2, Pp 385-403 (2017)
A new numerical model has been developed that makes it possible to describe the process of formation of a dyke of a combined composition on the basis of the dynamics of a viscous compressible fluid. The numerical thermo‐mechanical model shows the p
Externí odkaz:
https://doaj.org/article/d9286df9957b4c46bf5f9c6f6c22e84f
Autor:
D. V. Semenova, V.A. Yakovlev, R.A. Shelepaev, S. N. Rudnev, I. V. Karmysheva, V. G. Vladimirov
Publikováno v:
Russian Geology and Geophysics. 60:720-734
—The Bayan-Kol gabbro–granite association has been recognized within the West Sangilen fragment of collision zone in the northwestern framing of the Tuva–Mongolian massif, and its composition, age, and tectonic and geodynamic settings have been
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b0d845629188b4fe9b199ae9b82e4560
https://doi.org/10.15372/rgg2019065
https://doi.org/10.15372/rgg2019065
Autor:
G. N. Burmakina, A.A. Tsygankov, I. V. Karmysheva, V.A. Yakovlev, M.D. Buyantuev, V. B. Khubanov, V. G. Vladimirov
Publikováno v:
Russian Geology and Geophysics. 60:45-66
—Composite dikes (mingling dikes) of Western Sangilen (southeastern Tuva) are believed to indicate a shift from tectonic contraction, related to the mountain fold system formation, to postcollisional extension that ended with the disintegration of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::461a39de96200a2217ddabbcd6aeda02
https://doi.org/10.15372/rgg2019004
https://doi.org/10.15372/rgg2019004
Publikováno v:
Petrology. 25:87-113
The problems of tectonic control of composition, size, and morphology of synkinematic crustal granitoids are discussed by the example of the Western Sangilen granites (South-East Tuva). Comparative analysis was performed for felsic bodies and massifs
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8cdc371344df6384035a734dc49e3de7
https://doi.org/10.1134/s0869591117010040
https://doi.org/10.1134/s0869591117010040
Publikováno v:
GEOLOGY AND MINERAL RESOURCES OF SIBERIA. :126-134
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4b1317d81ec47c2d595ec8ff4458cba
https://doi.org/10.20403/2078-0575-2016-2-126-134
https://doi.org/10.20403/2078-0575-2016-2-126-134
Publikováno v:
Russian Geology and Geophysics. 55:411-427
We consider the primary nature and sources of the protoliths of metamorphic rocks of the Kurai block located in the large Teletskoe–Kurai system of deep faults separating the Gorny Altai and West Sayan structures. It has been established that the p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cfb829b1f94698b7d85ac51b81750abd
https://doi.org/10.1016/j.rgg.2014.03.001
https://doi.org/10.1016/j.rgg.2014.03.001