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Journal of the Geological Society; January 1984; v. 141; no. 1; p. 137-145; DOI: 10.1144/gsjgs.141.1.0137
© 1984 Geological Society of London
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Article

Remnants of the Hercynian orogen along the 'Calabrian-Peloritan arc', southern Italy: a review

P. Atzori, P. Ferla, A. Paglionico, G. Piccarreta and A. Rottura

Remnants of the Hercynian orogen, disturbed by Alpine tectonics, occur widely along the ‘Calabrian-Peloritan arc’. Indications of former oceanic conditions, for example Palaeozoic ophiolites and original deep water sediments, are lacking. Metamorphism developed under intermediate to low pressure conditions; the post-metamorphic plutonism appears to be more compatible with intracontinental orogenic processes than with an active continental margin. The possible evolution of this segment of the Hercynian orogen is discussed.






JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
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