Mantle source of the 2.44–2.50-Ga mantle plume-related magmatism in the Fennoscandian Shield: eviden...
Mantle source of the 2.44–2.50-Ga mantle plume-related magmatism in the Fennoscandian Shield: evidence from Os, Nd, and Sr isotope compositions of the Monchepluton and Kemi intrusions
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Berlin/Heidelberg: Springer Berlin Heidelberg
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Language
English
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Publisher
Berlin/Heidelberg: Springer Berlin Heidelberg
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Scope and Contents
Contents
Significant PGE and Cr mineralization occurs in a number of 2.44–2.50-Ga mafic layered intrusions located across the Karelian and Kola cratons. The intrusions have been interpreted to be related to mantle plume activity. Most of the intrusions have negative ε
Nd
values of about −1 to −2 and slightly radiogenic initial Sr isotope compositions...
Alternative Titles
Full title
Mantle source of the 2.44–2.50-Ga mantle plume-related magmatism in the Fennoscandian Shield: evidence from Os, Nd, and Sr isotope compositions of the Monchepluton and Kemi intrusions
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Record Identifier
TN_cdi_proquest_miscellaneous_1855084481
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1855084481
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ISSN
0026-4598
E-ISSN
1432-1866
DOI
10.1007/s00126-016-0673-9
