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Petrology of mafic lavas within the Onega plateau, Central Karelia: evidence for 2.0 Ga plume-related continental crustal growth in the Baltic Shield

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http://pubman.mpdl.mpg.de/cone/persons/resource/persons101004

Hofmann,  A. W.
Geochemistry, Max Planck Institute for Chemistry, Max Planck Society;

http://pubman.mpdl.mpg.de/cone/persons/resource/persons100979

Haase,  K. M.
Geochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Puchtel, I. S., Arndt, N. T., Hofmann, A. W., Haase, K. M., Kröner, A., Kulikov, V. S., et al. (1998). Petrology of mafic lavas within the Onega plateau, Central Karelia: evidence for 2.0 Ga plume-related continental crustal growth in the Baltic Shield. Contributions to Mineralogy and Petrology, 130, 134-153.


Cite as: http://hdl.handle.net/11858/00-001M-0000-0014-98EC-7
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