Tectonic evolution, volcanic features and geochemistry of the Paleoproterozoic Salla belt, northern Fennoscandia: From 2.52 to 2.40 Ga LIP stages to ca. 1.92–1.90 Ga collision-Reference-Cited by-同舟云学术

Tectonic evolution, volcanic features and geochemistry of the Paleoproterozoic Salla belt, northern Fennoscandia: From 2.52 to 2.40 Ga LIP stages to ca. 1.92–1.90 Ga collision

Published:2022-04 Issue: Volume:371 Page:106597
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Köykkä J.,Lahtinen R.,Manninen T.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

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4. Large igneous provinces, delamination, and fertile mantle;Anderson;Elements,2005

5. New paleomagnetic evidence from the early Proterozoic (2.5–2.4 Ga) Mount Generalskaya and Imandra layered intrusions, Kola Peninsula. Izvestiya;Arestova;Phy. Solid Earth,2002

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