Tracing Proterozoic arc mantle Hf isotope depletion of southern Fennoscandia through coupled zircon U–Pb and Lu–Hf isotopes-Reference-Cited by-同舟云学术

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Tracing Proterozoic arc mantle Hf isotope depletion of southern Fennoscandia through coupled zircon U–Pb and Lu–Hf isotopes

Published:2017-07 Issue: Volume:284-285 Page:122-131
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Petersson Andreas,Bjärnborg Karolina,Scherstén Anders,Gerdes Axel,Næraa Tomas

Funder

Royal Physiographic Society in Lund

Geologic Field Club in Lund

Geological Survey of Sweden

Swedish Research Council

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference52 articles.

1. Transitioning from Svecofennian to Transcandinavian Igneous Belt (TIB) magmatism in SE Sweden: implications from the 1.82Ga Eksjö tonalite;Åhäll;GFF,2002

2. Neodymium isotope systematics of the mantle beneath the Baltic shield: evidence for depleted mantle evolution since the Archaean;Andersen;Lithos,1995

3. Granitic magmatism by melting of juvenile continental crust: new constraints on the source of Palaeoproterozoic granitoids in Fennoscandia from Hf isotopes in zircon;Andersen;Journal of the Geological Society, London,2009

4. 1.8Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment;Andersson;Lithos,2006

5. Characterization of the Paleoproterozoic mantle beneath the Fennoscandian Shield: geochemistry and isotope geology (Nd, Sr) of c. 1.8Ga mafic plutonic rocks from the Transscandinavian Igneous Belt in southeast Sweden;Andersson;International Geology Review,2007

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