Detailed geological mapping paired with meso to microstructural analyses pointed out the presence, in the Lodè-Mamone Ortogneiss Complex (Baronie, North-eastern Sardinia), of two folds systems developed during the third deformation phase overprinting older D2 antiforms and synforms. These systems of fold are characterized by axes trending respectively WNW-ESE and SW-NE and steeply dipping axial planes. As a result of this study, the structure, previously interpreted as a simpler second phase-related antiform, can be better explained as the result of interference pattern between the second and the third phase-related fold systems. Greater lithological complexity can be observed also in the acid orthoderivate complex, resulting from metamorphism on a series of Ordovician granitoid intrusions.
|Autori interni:||MONTOMOLI, CHIARA|
|Autori:||CAROSI R.; FRASSI C.; MAGI S.; MONTOMOLI C.|
|Titolo:||Analisi strutturale dell’antiforme di Lodè-Mamone (Sardegna nord-orientale): un esempio di intereferenza complessa a scala chilometrica nl basamento Ercinico sardo|
|Anno del prodotto:||2005|
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