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