Isotopic analysis of five large books of muscovite from a pegmatite emplaced between the third and fourth deformational phases of the Svecokarelian orogenic episode indicate crystallization before 1880 m.y. with regional temperatures remaining elevated for about 120 m.y. The data are used to assess the validity of correlating deformational phases on the basis of structural evidence
White micas from the Penninic units of the Urtier Valley, in the Western Alps, have been dated by th...
The Lentiira-Kuhmo-Kostomuksha triangle, along the Finland – Russian border and within the central p...
Abstract: Rb–Sr dating of sub-closure temperature, syn-deformationly crystallized white micas from t...
Rb-Sr age determination on mica and whole-rock samples and K-Ar age determination on hornblendes wer...
The Suomusjärvi shear zone in the West Uusimaa area in the Proterozoic Svecofennides of SW Finland b...
Large (2 - 3 cm) crystals of ferroan pargasite in a narrow pegmatite vein that cross-cuts amphibolit...
In an effort to quantify the time parameter in the tectonomagmatic evolution of what has been called...
Four rock samples were collected from the crustal-scale South Finland shear zone in or-der to compar...
The Mäntylä complex is part of the extensive Central Finland Granitoid Complex. The intrusive sequen...
Four rock samples were collected from the crustal-scale South Finland shear zone in order to compare...
The Brazil Lake pegmatite of southwestern Nova Scotia is a rare example of Li-Cs-Ta (LCT) -type pegm...
<p>Muscovite B4M, distributed in 1961 as an age standard, was ground under ethanol. Five grain size ...
A tonalite-granodiorite-granite suite emplaced during the late Archaean D3 deformational phase yield...
The Lentiira-Kuhmo-Kostomuksha triangle, along the Finland – Russian border and within the central p...
International audienceIn order to date low-temperature deformation, intensely trained muscovite porp...
White micas from the Penninic units of the Urtier Valley, in the Western Alps, have been dated by th...
The Lentiira-Kuhmo-Kostomuksha triangle, along the Finland – Russian border and within the central p...
Abstract: Rb–Sr dating of sub-closure temperature, syn-deformationly crystallized white micas from t...
Rb-Sr age determination on mica and whole-rock samples and K-Ar age determination on hornblendes wer...
The Suomusjärvi shear zone in the West Uusimaa area in the Proterozoic Svecofennides of SW Finland b...
Large (2 - 3 cm) crystals of ferroan pargasite in a narrow pegmatite vein that cross-cuts amphibolit...
In an effort to quantify the time parameter in the tectonomagmatic evolution of what has been called...
Four rock samples were collected from the crustal-scale South Finland shear zone in or-der to compar...
The Mäntylä complex is part of the extensive Central Finland Granitoid Complex. The intrusive sequen...
Four rock samples were collected from the crustal-scale South Finland shear zone in order to compare...
The Brazil Lake pegmatite of southwestern Nova Scotia is a rare example of Li-Cs-Ta (LCT) -type pegm...
<p>Muscovite B4M, distributed in 1961 as an age standard, was ground under ethanol. Five grain size ...
A tonalite-granodiorite-granite suite emplaced during the late Archaean D3 deformational phase yield...
The Lentiira-Kuhmo-Kostomuksha triangle, along the Finland – Russian border and within the central p...
International audienceIn order to date low-temperature deformation, intensely trained muscovite porp...
White micas from the Penninic units of the Urtier Valley, in the Western Alps, have been dated by th...
The Lentiira-Kuhmo-Kostomuksha triangle, along the Finland – Russian border and within the central p...
Abstract: Rb–Sr dating of sub-closure temperature, syn-deformationly crystallized white micas from t...