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Volumn 286, Issue 5446, 1999, Pages 1928-1934

A lower mantle source for central European volcanism

Author keywords

[No Author keywords available]

Indexed keywords

CENOZOIC; MANTLE SOURCE; RIFTING; SEISMIC TOMOGRAPHY; VELOCITY STRUCTURE; VOLCANISM;

EID: 0033521134     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.286.5446.1928     Document Type: Article
Times cited : (221)

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    • The excess temperatures of plumes have been estimated to be 75 to 300°C in the upper mantle and 150 to 300°C in the lower mantle (19, 28).
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    • note
    • We thank M. Rehkämper for discussions on the geochemical signature of plumes and two reviewers for their critical reading of our manuscript Funding was provided by the NEESDI program (NWO grant 750-29-601) (S.G.) and the Netherlands Geoscience Foundation (GOA) (H.B.), both financially supported by the Netherlands Organization for Scientific Research (NWO), and by the Vening-Meinesz Research School of Geodynamics.


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