| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9532015 | Lithos | 2005 | 22 Pages |
Abstract
The geodynamic model which most satisfactorily explains our geological and geochemical observations is the formation of the Karelian sanukitoids in a cratonic environment adjacent to the Belomorian-Karelian suture.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
S.B. Lobach-Zhuchenko, H.R. Rollinson, V.P. Chekulaev, N.A. Arestova, A.V. Kovalenko, V.V. Ivanikov, N.S. Guseva, S.A. Sergeev, D.I. Matukov, K.E. Jarvis,