There are differences in the style of collisional orogens between the Phanerozoic and the
Precambrian, most notably the appearance of blueschists and ultrahigh pressure …

A comparative study of the central and southern parts of the Palaeoproterozoic
Svecofennian orogen in the Baltic/Fennoscandian Shield and the platform area to the east …

Baltica, in the core of the supercontinent Nuna, comprises Fennoscandia, Sarmatia and
Volgo-Uralia. We develop a tectonic model of Paleoproterozoic Fennoscandia based on …

A number of polymetallic vein mineralizations of different styles and metal associations,
including base, alloy, noble and critical metals, have been discovered around the …

Abstract The Paleoproterozoic oroclines of Fennoscandia played a vital role in the making of
continental equidimensional crust during the Svecofennian orogeny. We propose that the …

Global WGM-12 gravity and EMAG2v3 magnetic models were used to present new
information of the Estonian crust. The Estonian Precambrian crystalline basement …

Abstract The Svecofennian orogeny in Fennoscandia is an example of a long-lived orogeny
characterised by low pressure, high temperature (LP–HT) metamorphism. In this paper, we …

Evidence is presented for the crystallization age (ca. 1066–1033 Ma) and origin of the Lyon
Mountain Granite (formerly Lyon Mountain Gneiss), a widespread magnetite-bearing …

We have identified two contrasting styles of Paleoproterozoic metamorphism in the northern
part of the Fennoscandian Shield. The Karelia and Lapland-Kola Provinces, comprising …

The Estonian Precambrian crystalline basement, which consists of Paleoto Meso-
Proterozoic metamorphic and igneous rocks, is covered by a 100-780 m thick deposit of …