1.8 Ga magmatism in southern Finland: strongly enriched mantle and juvenile crustal sources in a post-collisional setting-Reference-Cited by-同舟云学术

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1.8 Ga magmatism in southern Finland: strongly enriched mantle and juvenile crustal sources in a post-collisional setting

Published:2010-07-23 Issue:14 Volume:53 Page:1622-1683
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Rutanen Henrikki¹,Andersson Ulf B.²,Väisänen Markku³,Johansson Åke⁴,Fröjdö Sören¹,Lahaye Yann⁵,Eklund Olav³

Affiliation:

1. a Geology & Mineralogy , Åbo Akademi University , Turku, Finland

2. b Department of Earth Sciences , Uppsala University , Uppsala, Sweden

3. c Department of Geology , University of Turku , Turku, Finland

4. d Laboratory for Isotope Geology , Swedish Museum of Natural History , Stockholm, Sweden

5. e The Finland Isotope Geosciences Laboratory , Geological Survey of Finland , Espoo, Finland

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2010.496241

Reference295 articles.

1. Growth-related 1.85–1.55 Ga magmatism in the Baltic Shield; a review addressing the tectonic characteristics of Svecofennian, TIB 1-related, and Gothian events

2. Intracratonic Palaeoproterozoic granitoids in northern Finland: Prolonged and episodic crustal melting events revealed by Nd isotopes and U-Pb ages on zircon

3. Granitic magmatism by melting of juvenile continental crust: new constraints on the source of Palaeoproterozoic granitoids in Fennoscandia from Hf isotopes in zircon

4. Granitoid episodes and mafic-felsic magma interaction in the Svecofennian of the Fennoscandian Shield, with main emphasis on the ∼1.8 Ga plutonics

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