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Isoclinal F1 synform refolded by F2 open folds (type 3 interference pattern) in white quartzites containing phengite, glaucophane and garnet. F1 folds developed under high-pressure metamorphic conditions. Morteda-Farinole eclogite Unit.
Locality Accendipipa, Corse (France)
PhotoID232

Field Trip Guidebook vol. 4, P27, ISPRA (2004) – 32nd INTERNATIONAL GEOLOGICAL CONGRESS, Florence, Italy.

Isoclinal F1 synform refolded by F2 open folds (type 3 interference pattern) in white quartzites containing phengite, glaucophane and garnet. F1 folds developed under high-pressure metamorphic conditions. Morteda-Farinole eclogite Unit.
Locality Accendipipa, Corse (France)
PhotoID232

Field Trip Guidebook vol. 4, P27, ISPRA (2004) – 32nd INTERNATIONAL GEOLOGICAL CONGRESS, Florence, Italy.

Photograph: R. Carosi