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Type-3 interference pattern between F1 southwest-facing F1 folds and F2 upright to north-verging F2 folds in Paleozoic quartzites and black shale involved in the Variscan Orogeny; Nurra Peninsula (Sardinia, Italy).
PhotoID683

Type-3 interference pattern between F1 southwest-facing F1 folds and F2 upright to north-verging F2 folds in Paleozoic quartzites and black shale involved in the Variscan Orogeny; Nurra Peninsula (Sardinia, Italy).
PhotoID683

Photograph: R. Carosi

Reference: CAROSI R. & OGGIANO G. (2002) – Transpressional deformation in northwestern Sardinia (Italy): insights on the tectonic evolution of the Variscan belt. Comptes Rendus Geoscience, 334, 287-294, Elsevier, Paris 2002. MONTOMOLI C. (2002) – Zone di taglio fragili-duttili nel basamento Varisico metamorfico di basso grado della Nurra meridionale (Sardegna nord-occidentale). Atti della Società Toscana di Scienze Naturali, Memorie seria A, 108, 23-29. CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. In: (eds.) Köhn, D., and De Paor, D., General Contributions 2006, Journal of the Virtual Explorer, Electronic Edition, ISSN 1441-8142, Volume 22, Paper 3.