Results 71 to 80 of about 1,083 (190)

Tectonic Evolution and Structural Control of Dike-Hosted Orogenic Gold Deposits in the Yana–Kolyma Collision Orogen (Eastern Siberia): Insights from the Eastern Margin of the Siberian Craton

open access: yesGeosciences
The Yana–Kolyma collision orogen, Eastern Siberia, is one of world-class gold economic belts, where large gold deposits are localized, mainly in the Upper Paleozoic and Lower Mesozoic clastic rocks.
Valery Yurievich Fridovsky   +1 more
doaj   +1 more source

Eclogite induced deformation of the siberian craton

open access: yes, 2020
The deformation of the cratons, whose roots are approximately 250 km deep is very difficult. The removal of the mantle lithosphere, which is one of the proposed mechanisms for the deformation of the craton that is stable for long periods, is carried out by many different processes. Deformation of the craton as a result of a gravitational instability is
openaire   +1 more source

EARLY NEOPROTEROZOIC GRANITOIDS IN THE RYAZANOVSKY MASSIF OF THE YENISEI RIDGE AS INDICATORS OF THE GRENVILLE OROGENY AT THE WESTERN MARGIN OF THE SIBERIAN CRATON

open access: yesГеодинамика и тектонофизика
Studies of the geological history of the Yenisei Ridge are important not only for understanding the tectonic evolution of mobile belts at the boundaries of ancient cratons but also for problem solving whether the Siberian craton was a part of the Rodinia
A. D. Nozhkin   +3 more
doaj   +1 more source

Geochronology of sillimanite-cordierite gneiss Atamanovo series of the South Yenisei Ridge (Russia)

open access: yesЛитосфера, 2017
The paper provides justification of Paleo Archaean age (3221 ± 15 Ma) of the granulite plutonic metamorphism that formed the Kan metamorphic complex of the Archaean crust in the Angara-Kan block of the Siberian craton. The age was defined on the basis of
A. M. Sazonov   +6 more
doaj   +2 more sources

Evidence of Subducted Archean Nitrogen in the Siberian Craton [PDF]

open access: yesGoldschmidt Abstracts, 2020
Peter H Barry, Michael Broadley
openaire   +1 more source

The evolution of the Siberian craton, petrogenesis and diamond potential of the mantle magmatic systems

open access: yesGeodynamics & Tectonophysics, 2014
The article reviews the history, main scientific fields and major results of the studies performed by the Laboratory of Petrology, Geochemistry and Ore Genesis and the Laboratory of Geology and Magmatism of Ancient Platforms.
P. I. Dorogokupets, K. N. Egorov
openaire   +3 more sources

THE SOUTHERN FRAGMENT OF THE SIBERIAN CRATON: “LANDSCAPE” HISTORY OVER TWO BILLION YEARS

open access: yesГеодинамика и тектонофизика, 2015
In the state-of-the-art geology, concepts of evolution of interrelated geodynamic and biotic events throughout the history of the Earth have been developed (Fig. 1). Research results on sediments, bio-stratigraphy and geodynamics of the southern fragment
Arkady M. Stanevich   +4 more
doaj   +1 more source

Phanerozoic mafic magmatism in the southern Siberia craton: geodynamic implications

open access: yes, 2010
The Phanerozoic history of mafic magmatism in the southern Siberian craton included three major events. The earliest event (∼500 Ma) recorded in dolerite dikes occurred during accretion and collision at the early stage of the Central Asian orogen ...
D.P. Gladkochub   +13 more
core   +1 more source

P-T path of metamorphism and U-Pb monazite and zircon age of the Kitoy terrane: Implication for Neoarchean collision in SW Siberian Craton

open access: yes, 2020
The first data on P-T metamorphic conditions coupled with U-Pb monazite and zircon age obtained for the Neoarchean Kitoy granulite-gneiss terrane (SW Siberian Craton). Alumina gneisses of the Kitoy terrane indicate two-staged metamorphic evolution.
Savel'eva, Valentina B.   +3 more
core   +1 more source

Features of the impurity composition of diamonds from placers of the northeastern Siberian craton

open access: yesДоклады Академии наук, 2019
Diamond crystals from the Istok (25 crystals) and Mayat (49 crystals) placers were studied using the EPR-, IR-, and luminescence methods. The total content of impurity nitrogen in forms of A-, B-, and C (P1)-centers ranges from 50 to 1200 ppm. According to the EPR-spectroscopy, the presence of nitrogen C(P1), N3V nitrogen-titanium OK1, N3, NU1 impurity
V. S. Shatsky   +4 more
openaire   +2 more sources

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