© Patrick CORDIER/CNRS Images
Reference
20080001_0184
Dislocations dans la wadsleyite MgSiO4, un polymorphe de haute pression stable dans la zone de trans
Dislocations dans la wadsleyite MgSiO4, un polymorphe de haute pression stable dans la zone de transition du manteau terrestre entre 470 et 520 km de profondeur. L'image de microscopie électronique en transmission montre des défauts cristallins (dislocations) responsables de la déformation de ce minéral.
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