The “intraorogenic” Svecofennian Herräng mafic dyke swarm in east-central Sweden: age, geochemistry and tectonic significance
Author:
Affiliation:
1. Department of Geosciences, Swedish Museum of Natural History, Stockholm, Sweden
Publisher
Informa UK Limited
Subject
Paleontology,Geology
Link
https://www.tandfonline.com/doi/pdf/10.1080/11035897.2019.1708450
Reference54 articles.
1. Characterization of the Paleoproterozoic Mantle beneath the Fennoscandian Shield: Geochemistry and Isotope Geology (Nd, Sr) of ~ 1.8 Ga Mafic Plutonic Rocks from the Transscandinavian Igneous Belt in Southeast Sweden
2. Short-lived mantle generated magmatic events and their dyke swarms
3. Source character, mixing, fractionation and alkali metasomatism in Palaeoproterozoic greenstone dykes, Dannemora area, NE Bergslagen region, Sweden
4. Neodymium isotopes in the Colorado Front Range and crust–mantle evolution in the Proterozoic
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1. On the origin and evolution of the 1.86–1.76 Ga Mid-Baltic Belt in the western East European Craton;Precambrian Research;2021-12
2. Tracing arclogites in the Paleoproterozoic Era – A shift from 1.88 Ga calc-alkaline to 1.86 Ga high-Nb and adakite-like magmatism in central Fennoscandian Shield;Lithos;2020-11
3. The Paleoproterozoic Hedesunda granite complex, east-central Sweden, a composite intrusion;International Journal of Earth Sciences;2020-07-02
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