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TítuloForms and structural fabric in granite rocks

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Fig. 1. Different spheroidal disjunction structures corresponding to igneous rocks. a) Phonolite from Gran Canaria, Spain; b) Granite from La Alberca, Salamanca, Spain (photo by courtesy of M
Fig. 1. Different spheroidal disjunction structures corresponding to igneous rocks. c) Granite from Los Riojanos, Pampa de Achala, Argentina; d) Granite from Platja d’Aro, Girona, Spain.
Fig. 3. Sheeting in granite rock intersecting the magmatic fabric (schlieren) from Maríz, Coruña Spain.
Fig. 5. Pseudobedding in granite rock from Gmünd, Lower Austria. (by courtesy of K.H.Hubber).
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