Zobrazeno 1 - 10
of 33
pro vyhledávání: '"M. V. Mints"'
Autor:
M. V. Mints, K. A. Dokukina
Publikováno v:
Геодинамика и тектонофизика, Vol 12, Iss 3, Pp 662-667 (2021)
In their research, the authors of the comments have focused on the Late Paleoproterozoic rims of zircons, but ignored many important details of their own data. Their comments are based on a misconception that eclogite zircons have unique geochemical
Externí odkaz:
https://doaj.org/article/2489328766764bb6a0899164e203c9fe
Autor:
M. V. Mints, K. A. Dokukina
Publikováno v:
Геодинамика и тектонофизика, Vol 11, Iss 1, Pp 151-200 (2020)
A critical discussion of competing models of the geodynamic nature (oceanic or continental subduction) and age (Meso-Neoarchean or Late Paleoproterozoic) of the eclogite facies metamorphism in the Belomorian eclogite province (BEP) is based on the sy
Externí odkaz:
https://doaj.org/article/a6e63436f8d44ecba6fb9380e467ec8c
Autor:
M. V. Mints, T. B. Afonina
Publikováno v:
Геодинамика и тектонофизика, Vol 9, Iss 2, Pp 309-363 (2018)
The structure of the Archaean crust of the North America has been studied based on the synthesis of geolo‐ gical and geophysical data, including seismic sections along LITHOPROBE Geotransects, magnetic and gravity anomaly maps, and seismic tomograp
Externí odkaz:
https://doaj.org/article/16667f58141b4a3eb7c2656c0fff6c6c
Autor:
M. V. Mints
Publikováno v:
Геодинамика и тектонофизика, Vol 8, Iss 3, Pp 619-642 (2017)
The objective of this paper is to represent the main features inherent to Grenville-Sveconorwegian Orogen (GSNO) and to propose a model of tectonic and geodynamic evolution of this orogen based on the results of research concerning similar Precambria
Externí odkaz:
https://doaj.org/article/3b8895f7fb7446f582bc1c2daf57a16a
Autor:
M. V. Mints, P. G. Eriksson
Publikováno v:
Геодинамика и тектонофизика, Vol 7, Iss 2, Pp 173-232 (2016)
Paradoxically, the lists of “proxies” of both plate- and plume-related settings are devoid of even a mention of the high-grade metamorphic rocks (granulite, amphibolite and high-temperature eclogite facies). However, the granulite-gneiss belts an
Externí odkaz:
https://doaj.org/article/7bb711e1ff1841eda55edcbbc3c31659
Publikováno v:
Геодинамика и тектонофизика, Vol 5, Iss 3, Pp 717-742 (2015)
The article presents new data on the deep crustal structure, origin and evolution of the Bryansk-Kursk-Voronezh orogen in the south-eastern segment of the East European craton; it is composed of the Paleoproterozoic formations and areas of reworked A
Externí odkaz:
https://doaj.org/article/c3fa41311a5d4afbac517bfa928a5d1d
Publikováno v:
Геодинамика и тектонофизика, Vol 6, Iss 2 (2015)
The complex geophysical 3D model of the Earth's crust and the upper mantle is created for the Archaean Karelian Craton and the Late Palaeoproterozoic accretionary Svecofennian Orogen of the southeastern Fennoscandian Shield with the use of methods of
Externí odkaz:
https://doaj.org/article/535855e51e834cbbacc9c67c7b67aacc
Autor:
K. A. Dokukina, M. V. Mints
Publikováno v:
Geodinamika i Tektonofizika, Vol 12, Iss 3, Pp 662-667 (2021)
In their research, the authors of the comments have focused on the Late Paleoproterozoic rims of zircons, but ignored many important details of their own data. Their comments are based on a misconception that eclogite zircons have unique geochemical
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::10507501feae6d3f056a7a44edb7875f
https://www.gt-crust.ru/jour/article/view/1246
https://www.gt-crust.ru/jour/article/view/1246
