Browsing Royal Museum for Central Africa by Author "Bolle, O."
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The Farsund intrusion (SW Norway): A marker of Late-Sveconorwegian (Grenvillian) tectonism emplaced along a newly defined major shear zone.
Bolle, O.; Diot, H.; Liégeois, J.P.Vander Auwera, J. et al. -
The fast evolution of a crustal hot zone at the end of a transpressional regime: the Saint-Tropez peninsula granites and related dykes (Maures Massif, SE France).
Duchesne, J.C.; Liégeois, J.P.; Vander Auwera, J.Bolle, O.Bruguier, O.Matukov, D.I.Sergeev, S.A. et al.