Origin and geodynamic evolution of the Archean crust of eastern Finland

The Archaean crust of eastern Finland is composed of three main lithological units: ‒ Gneissic basement. It was originally composed of tonalites, trondhjemites and granodiorites emplaced at 2.86 G.a. and 2.62 G.a. and subsequently transformed into grey gneisses. The parental magmas originated from t...

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Bibliografische gegevens
Hoofdauteurs: H. Martin, B. Auvray, S. Blais, R. Capdevila, J. Hameurt, B.M. Jahn, D. Piquet, G. Quérré, Ph. Vidal
Formaat: Artikel
Taal:English
Gepubliceerd in: Geological Society of Finland 1984-12-01
Reeks:Bulletin of the Geological Society of Finland
Onderwerpen:
Online toegang:http://www.geologinenseura.fi/bulletin/Volume56/sgs_bt_056_pages_135_160.pdf