Strain localization via mechanical mixing and metasomatism: an example from the metagabbros of Marine de Giottani, Alpine Corsica, France

De la géologie structurale à la géodynamique : un numéro thématique dédié à la contribution de l’école rennaise de tectonique - Hommage à J-P Brun, P. Choukroune et P.R. Cobbold

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Fig. 6

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a. ACF diagram representing the composition of the three rock types considered: metagabbros, schists and serpentinite. A is corrected for sodium and potassium (A = Al₂O₃ - Na₂O − K₂O), C is corrected for phosphorus (C = CaO − P₂O₃) and F is corrected for manganese and titanium (F = FeO_t+ MgO − MnO − TiO₂ with FeO_t= 0.8998 × Fe₂O₃). b. Binary diagram representing the trend of Al2O3 vs TiO2 in the bulk rocks.

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