HR: 0800h
AN: V21D-0631    [Abstracts]
TI: Relationships between tectonism, volcano-tectonism and volcanism: the Ischia island (Italy) case.
AU: * Marotta, E
EM: marotta@ov.ingv.it
AF: INGV-Osservatorio Vesuviano, via Diocleziano 328, Napoli, 80124 Italy
AU: de Vita, S
EM: devita@ov.ingv.it
AF: INGV-Osservatorio Vesuviano, via Diocleziano 328, Napoli, 80124 Italy
AU: Orsi, G
EM: orsi@ov.ingv.it
AF: INGV-Osservatorio Vesuviano, via Diocleziano 328, Napoli, 80124 Italy
AU: Sansivero, F
EM: sansivero@ov.ingv.it
AF: INGV-Osservatorio Vesuviano, via Diocleziano 328, Napoli, 80124 Italy
AB: The resurgent calderas of Ischia, Campi Flegrei and Pantelleria are characterized by differentially displaced blocks, and distribution of later eruption vents in a well defined sector of the resurgent area. These features suggest a simple shearing block resurgence mechanism. Moreover, the studies carried out on Ischia and Campi Flegrei evidenced a very complex structural pattern due to deformation related to the local stress regime induced by magmatism and volcanism and also to reactivation of regional structures. In order to better define the relationships among tectonic, volcano-tectonic and caldera resurgence mechanism, a structural study has been carried out at Ischia, where the Mt. Epomeo has been uplifted of about 900 m in the past 30 ka. The measures taken on 1,400 planar surfaces (faults, joints and fracture cleavages) show that the resurgent area is composed of differentially displaced blocks whose uplifting is maximum for the Mt. Epomeo and decreases southeastward. The resurgent area has a poligonal shape resulting from the reactivation of regional faults and by the activation of faults directly related to volcano-tectonism. The limit of the resurgent area is not defined towards the north, as beach deposits displaced at variable elevation by E-W and NW-SE trending faults, are exposed along the coastline. The western sector is bordered by inward-dipping, high-angle reverse faults, whose directions vary from N40E to NS and N50W from NW to SW of the block, testifying a compressional stress regime active in this area. These features are cut by late outward-dipping normal faults due to gravitational readjustment of the slopes. Vertical faults border the block at NE ad SW with right transtensive and left transpressive movements, respectively. The area located to the east of the most uplifted block, characterized by a tensile stress regime, has been deformed by N-S, N40-70E and N15W trending normal faults, with maximum elongation direction along N50W. The results of our study and the volcanological data of the past 3 ka, suggest that the eastern part of the resurgent block is the area with highest probability of vent opening in case of renewal of volcanism. Occurrence of landslides just before and after eruptions, suggest that resurgence occurs through discontinuous vertical movements which likely trigger the volcanic activity.
DE: 8175 Tectonics and landscape evolution
DE: 8178 Tectonics and magmatism
SC: Volcanology, Geochemistry, Petrology [V]
MN: Fall Meeting 2005