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

Puchtel, I. S.; Arndt, N. T.; Hofmann, A. W.; Haase, K. M.; Kröner, A.; Kulikov, V. S.; Kulikova, V. V.; Garbe-Schönberg, C.-D.; Nemchin, A. A.

Item

ITEM ACTIONSEXPORT

Add to Basket

Local TagsRelease HistoryDetailsSummary

Released

Journal Article

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

MPS-Authors

/persons/resource/persons101004

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

/persons/resource/persons100979

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

External Resource

No external resources are shared

Fulltext (restricted access)

There are currently no full texts shared for your IP range.

Fulltext (public)

There are no public fulltexts stored in PuRe

Supplementary Material (public)

There is no public supplementary material available

Citation

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

Abstract

There is no abstract available