Lithospheric mantle beneath the south-eastern Siberian craton: petrology of peridotite xenoliths in...
Lithospheric mantle beneath the south-eastern Siberian craton: petrology of peridotite xenoliths in basalts from the Tokinsky Stanovik
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Heidelberg: Springer Nature B.V
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Language
English
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Publisher
Heidelberg: Springer Nature B.V
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We provide petrographic, major and trace element data for over 30 spinel peridotite xenoliths from the Tokinsky Stanovik (Tok) volcanic field on the Aldan shield to characterize the lithospheric mantle beneath the south-eastern margin of the Siberian craton, which formed in the Mesoproterozoic. High equilibration temperatures (870-1,010 degrees C)...
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Full title
Lithospheric mantle beneath the south-eastern Siberian craton: petrology of peridotite xenoliths in basalts from the Tokinsky Stanovik
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TN_cdi_proquest_journals_208189852
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_208189852
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ISSN
0010-7999
E-ISSN
1432-0967
DOI
10.1007/s00410-005-0672-9
