Relicts of Paleoproterozoic LIPs in the Belomorian province, eastern Fennoscandian Shield: barcode reconstruction for a deeply eroded collisional orogen

Geological, geochemical, isotopic and geochronological data for Paleoproterozoic mafic intrusions and dykes indicate that distinct magmatic events dated at c. 2.50, 2.45, 2.40, 2.30, 2.23 and 2.12 Ga can be distinguished in the Belomorian Province, Eastern Fennoscandian Shield. The similarity of Pal...

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Bibliographic Details
Main Authors: Stepanova, Alexandra, S. Stepanov, Vladimir, N. Larionov, Alexander, B. Salnikova, Ekaterina, V. Samsonov, Alexander, Azimov, Pavel, V. Egorova, Svetlana, I. Babarina, Irina, O. Larionova, Yulia, A. Sukhanova, Maria, V. Kervinen, Anna, A. Marksimov, Oleg
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of London 2021
Subjects:
Geology
FOS Earth and related environmental sciences
Fennoscandian
karelian
Lapland
Online Access:https://dx.doi.org/10.6084/m9.figshare.c.5490941.v1
https://geolsoc.figshare.com/collections/Relicts_of_Paleoproterozoic_LIPs_in_the_Belomorian_province_eastern_Fennoscandian_Shield_barcode_reconstruction_for_a_deeply_eroded_collisional_orogen/5490941/1
Description
Summary:Geological, geochemical, isotopic and geochronological data for Paleoproterozoic mafic intrusions and dykes indicate that distinct magmatic events dated at c. 2.50, 2.45, 2.40, 2.30, 2.23 and 2.12 Ga can be distinguished in the Belomorian Province, Eastern Fennoscandian Shield. The similarity of Paleoproterozoic magmatic barcodes for the Belomorian Province and Karelian Craton in the c. 2.5–2.1 Ga interval suggests a neighbouring position of these crustal segments in an Archean continent. Intensive tectonic and metamorphic reworking of mafic intrusions and dykes in the Belomorian Province during the c. 2.0–1.8 Ga Lapland–Kola orogeny produced differences in mineral assemblages and tectonic position in comparison with the Karelian Craton.

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