Results 121 to 130 of about 975 (179)

Sulfur and metal fertilization of the lower continental crust. [PDF]

open access: yesLithos, 2016
Locmelis M   +5 more
europepmc   +1 more source

SVECOFENNIAN ACREТION OROGEN: MODERN VIEWS ON ITS STRUCTURE AND EVOLUTION

open access: yesProceedings of the Karelian Research Centre of the Russian Academy of Sciences, 2022
openaire   +1 more source

Large-scale crustal growth driven by LIP magmatism during the Paleoproterozoic. [PDF]

open access: yesNat Commun
Simões MS   +6 more
europepmc   +1 more source

Tectonic setting shapes microbial biosynthetic potential across global geothermal environments

open access: yes
Pelliciari Silva AC   +18 more
europepmc   +1 more source

Isotope response to latent geological processes in the Belomorian and Svecofennian Mobile Belts

open access: yesProceedings of the Karelian Research Centre of the Russian Academy of Sciences
Shauket Baltybaev   +3 more
openaire   +1 more source

Chronology and geochemistry of late Svecofennian processes in northern Sweden

open access: yesGff, 1989
Abstract Radiometric and geochemical data have been used to characterize the concluding stages of the Svecofennian orogeny in northern Sweden. U-Pb zirzon ages of 1879±7 and 1858±9 Ma have been obtained from two unfoliated granitoids of the North Svecofennian Subprovince.
Torbjörn Skiöld, Björn Ohlander
exaly   +3 more sources

The accretionary Svecofennian orogen—insight from the BABEL profiles

open access: yesPrecambrian Research, 2005
Abstract The BABEL profiles B, C, 1–7 form a 1200 km long nearly continuous cross-section through the Svecofennides. The near-vertical marine reflection profiles display a wide range of crustal structures that can be associated with both the accretionary Svecofennian orogeny (1.96–1.75 Ga) and the following Subjotnian and Jotnian rift-stages (1.65–1 ...
Annakaisa Korja, Pekka Heikkinen
exaly   +4 more sources

The Svecofennian Orogen: a tectonic model

Precambrian Research, 1997
Abstract Recent geological studies have provided new concepts concerning the timing of the final break-up of the Archaean craton. Age data on detrital zircons from sedimentary rocks in Sweden and Finland show marked similarities and indicate pervasive homogenization of accumulated material.
Mikko Nironen
exaly   +2 more sources

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