A detailed structural analysis carried out on the volcanic products of the island of Pantelleria has shown that the large- scale setting is dominated by N-S trending normal faults and NW-SE right-lateral strike-slip faults, while mesostructural data show a more complex pattern which is characterized by 4 systems of discontinuity. A model is described that helps to understand the characters of the volcanism associated with a zone of continental collision as well as its distribution, which is not rigorously in accordance with a classical rifting process.-after Authors

Transtensive tectonics in the Strait of Sicily: structural and volcanological evidence from the island of Pantelleria.

CRISCI, Gino Mirocle;
1985-01-01

Abstract

A detailed structural analysis carried out on the volcanic products of the island of Pantelleria has shown that the large- scale setting is dominated by N-S trending normal faults and NW-SE right-lateral strike-slip faults, while mesostructural data show a more complex pattern which is characterized by 4 systems of discontinuity. A model is described that helps to understand the characters of the volcanism associated with a zone of continental collision as well as its distribution, which is not rigorously in accordance with a classical rifting process.-after Authors
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.11770/127475
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