Production year
1989
© Michel FAURE/CNRS Images
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Boudins d'amphibolite préservés dans des roches partiellement fondues ou migmatites. Noter l'obliquité entre la foliation des amphibolites et celle des migmatites. Les amphibolites correspondent à des "restites" n'ayant pas subi la fusion du fait de leur composition chimique ferro-magnésienne mais ayant connu une rotation rigide ultérieurement. Massif du Dabieshan, Province du Hubei, Chine.
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1989
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