This part of the field trip (Fig. 1) is devoted to observe the main geological feature of western Elba: i- Mt. Capanne intrusion, a monzogranitic magmatic body with associate dike swarms and microgranite masses and, ii- its thermometamorphic aureole consisting of several types of hornfels after the ophiolite succession.
C-Western Elba - The Monte Capanne Monzogranite / M. COLI; S. CONTICELLI; G. MORATTI; E. PANDELI; P. PAPINI; S. TOMMASINI. - In: OFIOLITI. - ISSN 0391-2612. - STAMPA. - 26:(2001), pp. 351-356. [10.4454/ofioliti.v26i2a.156]
C-Western Elba - The Monte Capanne Monzogranite
COLI, MASSIMO;CONTICELLI, SANDRO;PANDELI, ENRICO;TOMMASINI, SIMONE
2001
Abstract
This part of the field trip (Fig. 1) is devoted to observe the main geological feature of western Elba: i- Mt. Capanne intrusion, a monzogranitic magmatic body with associate dike swarms and microgranite masses and, ii- its thermometamorphic aureole consisting of several types of hornfels after the ophiolite succession.
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