Zobrazeno 1 - 10
of 26
pro vyhledávání: '"K. A. Dokukina"'
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:
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
Autor:
K. I. Dokukina
Publikováno v:
Plant Breeding and Seed Production. :59-68
Autor:
K. A. Dokukina, Michael V. Mints
Publikováno v:
Journal of Geodynamics. 123:1-37
A model of Mesoarchaean spreading ridge subduction and related metamorphism, magmatism and deformation in an active continental margin is presented here. The eclogites exposed along northeastern boundary of the Belomorian orogen in the eastern Fennos
Publikováno v:
Doklady Earth Sciences. 477:1353-1357
In the Salma eclogite of the Belomorian eclogite province, a dumortierite–phengite–corundum–bearing quartz–feldspar rock has been studied: its primary HP mineral paragenesis included garnet, phengite, and quartz. The phengite–quartz rocks w
Publikováno v:
Journal of Metamorphic Geology. 35:435-451
The eclogites exposed along northeastern boundary of the Belomorian orogen in the eastern Fennoscandian Shield were formed as a result of Mesoarchean–Neoarchean subduction and collision. As has been shown previously, the common protolith of the Sal
Publikováno v:
Tectonophysics. 799:228701
The oval-shaped basin of Hudson Bay occurs near the center of the round-oval Archaean crustal domain of the North American continent. This paper presents models of the geological structure and evolution of the subcontinental lithospheric mantle under
Autor:
T. V. Kaulina, Sergey G. Simakin, Elena N. Lepekhina, L. M. Natapov, Konstantin V. Van, A. N. Konilov, Michael V. Mints, K. A. Dokukina, Elena Belousova
Publikováno v:
Gondwana Research. 25:585-613
The Belomorian eclogite province was repeatedly affected by multiple deformation episodes and metamorphism under moderate to high pressure. Within the Gridino area, high pressure processes developed in a continental crust of tonalite–trondhjemite
Publikováno v:
Gondwana Research. 25:561-584
The aim of this paper is to review the main features of the Meso-Neoarchaean Belomorian eclogite province (BEP) in the northeastern Fennoscandian Shield, including regional and local geology, geochemistry, petrology and geochronology and to compare t