Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/7918| DC Field | Value | Language |
|---|---|---|
| dc.contributor.authorall | De Vita, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.authorall | Orsi, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.authorall | Di Vito, M. A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.authorall | Marotta, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.authorall | Sansivero, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.date.accessioned | 2012-03-26T10:24:24Z | en |
| dc.date.available | 2012-03-26T10:24:24Z | en |
| dc.date.issued | 2005 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/7918 | en |
| dc.description.abstract | The role of pre-existing tectonic structures and regional stress regime on the geometry of calderas is widely recognized in the more recent literature on this topic. In fact, although in many cases the shape of calderas is broadly circular at a great scale, a detailed study of the collapse structures, almost always evidences the presence of linear features inherited from the “pre-caldera” regional tectonic setting. These features, commonly visible in the outcropping rocks that form the pre-volcanic basement, also testify the regional stress field in which volcanism took place. A complete range of increasing complexity examples exists in nature, from elliptical calderas, with a variable degree of ellipticity, to fully irregular calderas, with large linear border sectors due to re-activation of pre-existing regional faults. Elliptical calderas are usually associated with continental rifting, in which regional extension is marked by different horizontal stress components. In these cases the elongation of calderas is parallel to the trend of the regional structures. In some other cases the elongation of the calderas is perpendicular or oblique to the rift structures. This suggests that additional factors may influence the formation of these calderas and the related magma chambers at depth. Examples of such transverse calderas are found along the oceanic ridge of Iceland and along the East African Rift System. Recent studies demonstrated that re-activation of pre-existing structures, orthogonal to the main rift direction, controlled migration and storage of magma bodies at depth, and conditioned activation of volcanism and caldera formation at shallower levels. These so-called transfer structures control the emplacement of surface magma chambers and magma extrusion mainly in that regions in which tectonism and deformational history are very complex, as in the case of the Apennine chain and the peri-Tyrrhenian area. Where multiple extensional systems intersects to each other, transverse depressions are formed, and volcanism is dominated by caldera-forming eruptions. In these cases it is well evident the control exerted by pre-existing regional structures on the geometry of calderas. Some of these calderas have been later affected by resurgence processes, in which the uplifted blocks are bordered by faults whose geometry is inherited by the pre-caldera regional tectonic setting. The Campi Flegrei caldera and the island of Ischia are good examples of complex, resurgent calderas, characterized by a non regular shape, with large linear rim sectors, for which it is possible to demonstrate the control exerted by pre-existing regional tectonic structures | en |
| dc.language.iso | English | en |
| dc.relation.ispartof | Acta Vulcanologica | en |
| dc.relation.ispartofseries | Special issue 1-2/17(2005) | en |
| dc.subject | Caldera collapse | en |
| dc.subject | Block resurgence | en |
| dc.subject | Regional tectonics | en |
| dc.subject | Volcano-tectonics | en |
| dc.title | THE ROLE OF PRE-EXISTING TECTONIC STRUCTURES ON THE GEOMETRY OF CALDERAS AND RESURGENT BLOCKS: A REVIEW | en |
| dc.type | article | en |
| dc.description.status | Published | en |
| dc.description.pagenumber | 9 -22 | en |
| dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneous | en |
| dc.relation.references | Abebe, T., Mazzarini, F., Innocenti, F., Manetti, P. (1998): The Yerer-Tullu Wellel volcanotectonic lineament: a transtensional structure in central Ethiopia and the associated magmatic activity. J. Afr. Earth Sci., 26, 135-150. Acocella, V., Funiciello, R. (2002): Transverse structures and volcanic activity along the Tyrrhenian margin of central Italy. Boll. Soc. Geol. It., Sp. Vol. 1, 739-747. Acocella, V., Korme, T. (2002): Holocene extension direction in the axial zone of the Main Ethiopian Rift. Terra Nova. In press. Acocella, V., Korme, T., Salvini, F., Funiciello, R. (2002): Elliptic calderas in the Ethiopian Rift: control of pre-existing structures. J. Volcanol. Geotherm. Res., 119, 189-203. Agip, 1987. Modello geotermico del sistema flegreo (Sintesi). Servizi Centrali per l'Esplorazione, SERG-MESG, San Donato, 23 pp. Barberi, F., Bonatti, E., Marinelli, G., Varet, J. (1974): Transverse tectonics durino the split of a continent: data from the Afar Rift. Tectonophysics, 23, 17-29. Barberi, F., E. Cassano, P. La Torre, Sbrana, A. (1991): Structural Evolution of Campi Flegrei Caldera in Light of Volcanological and Geophysical Data. J. Volcanol. Geotherm. Res., 48 (1/2), 33-49. Bartole, R. (1984): Tectonic Structures of the Latian-Campanian Shelf (Tyrrhenian Sea). Boll. Ocean. Teor. Appl., 2, 197,230. Begazzi, G., Bonadonna, F.P., Di Paola, G.M., Giuliani, A. (1981): New K-Ar and fission track ages of the last volcano-tectonic phase in the Ethiopian Rift Valley (Tullu Moye area). In: “Proceedings of the first international symposium on crustal movements in Africa”. A.M. Wassef (Ed.), 141-159. Bosworth, W., Burke, K., Strecker, M. (2000): Magma chamber elongation as an indicator of intraplate stress field orientation: “borehole breakout mechanism” and examples from the Late Pleistocene to Recent Kenia Rift Valley. In: “Stress, strain and structure, a volume in honour of W.D. Means”, M.W. Jessel and J.L. Urai (Eds.). J. Virtual Explor, 2. Brown, R.J., Orsi, G., de Vita, S. (2006): New insights into Late Pleistocene explosive volcanic activity and caldera formation on Ischia (southern Italy). Bull. Volcanol. (submitted). Carrara, E., Iacobucci, F., Pinna, E., Rapolla, A. (1973) . Gravity and magnetic survey of the Campanian volcanic area, S. Italy. Boll. Geof. Teor. Appl., 15 (57), 39, 51. Carrara, E., Iacobucci, F., Pinna, E., Rampolla, A. (1974): Interpretation of gravity and magnetic anomalies near Naples, Italy, using computer techniques. Bull. Volcanol. 38 (2), 458, 467. Chiodini, G., Avino, R., Brombach, T., Caliro, S., Cardellini, C., de Vita, S., Frondini, F., Marotta, E., Ventura, G. (2004). Fumarolic and diffuse soil degassing west of Mount Epomeo, Ischia (Italy). J. Volcanol. Geotherm. Res., 133, 291-309. Chorowicz, J., Collet, B., Bonaria, F.F., Korme, T. (1994): North-Northwest extension direction in the Ethipoian Rift deduced from the orientation of extension structures and fault-slip analysis. Geol. Soc. Am. Bull., 105, 1560-1570. Civetta, L., G. Orsi, L. Pappalardo, R. V. Fisher, G. Heiken, Ort, M. (1997): Geochemical Zoning, Mingling, Eruptive Dynamics and Depositional Processes - The Campanian Ignimbrite, Campi Flegrei Caldera, Italy, J. Volcanol. Geotherm. Res., 75, 183-219. Cole, J. W., (1969): Gariboldi volcanic complex, Ethiopia. Bull. Volcanol., 33, 566-578. Coussement, C., Gente, P., Rolet, J., Tiercelin, J.J., Wafula, M., Buku, S. (1994): The North Tanganyika hydrothermal fields, East African Rift system: their tectonic control and relationship to volcanism and rift segmentation. Tectonophysics, 237, 155-173. D’Antonio, M., Civetta, L., Orsi, G., Pappalardo, L., Piochi, M., Carandente, A., de Vita, S., Di Vito, M. A., Isaia, R., Southon, J. (1999): The present state of the magmatic system of the Campi Flegrei caldera based on the reconstruction of its behaviour in the past 12 ka. J. Volcanol. Geotherm. Res., 91, 247-268. D’Argenio, B., Pescatore, T., Scandone, P. (1973): Schema geologico dell’Appennino meridionale (Campania e Lucania). Atti Conv. Moderne vedute sulla geologia dell’Appennino. Roma. Acc. Naz. Lincei, q.183. Dawson, J.B. (1992): Neogene tectonics and volcanicity in the North Tanzania sector of the Gregory Rift Valley: constraints with the Kenya sector. Tectonophysics, 204, 81-92. De Chabalier,J.B., Avouac, J.P. (1994): Kinematics of the Asal Rift (Djibouti) detrmined from the deformation of Fieale volcano. Science, 265, 1677-1681. Deino, A.L., Orsi, G., Piochi, M., de Vita, S. (2003): The age of the Neapolitan Yellow Tuff caldera-forming eruption (Campi Flegrei caldera – Italy) assessed by 40Ar/39Ar dating method. J. Volcanol. Geotherm. Res., 133, 157-170. de Vita, S., Sansivero, F., Orsi, G., Marotta, E., Piochi, M. (2006a): Volcanological and structural evolution of the Ischia resurgent caldera (Italy) over the past 10 ka. AGS Book (submitted). de Vita S., Sansivero F., Orsi G., Marotta E. (2006b). Cyclical slope instability and volcanism related to volcano-tectonism in resurgent calderas: the Ischia island (Italy) case study. Eng. Geol. In press. Di Paola, G.M. (1972): The Ethiopian Rift Valley (between 7°00’N lat. And 8°40’N lat.). Bull Volcanol. 36, 317-560. Di Vito, M. A., Lirer, L., Mastrolorenzo, G., Rolandi, G. (1987). The Monte Nuovo eruption (Campi Flegrei, Italy). Bull. Volcanol., 49, 608-615. Druitt, T.H., Sparks, R.S.J. (1984): On the formation of calderas during ignimbrite eruptions. Nature, 310, 679-681. Faccenna, C., Funiciello, R., Bruni, A., Mattei, M., Cagnotti, L. (1994): Evolution of a transfer related basin: the Ardea basin (Latium, Central Italy). Basin Research, 6, 35-46. Fedele, F., Giaccio, B., Isaia, R., Orsi, G. (2003). The Campanian Ignimbrite eruption, Heinrich Event 4, and Palaeolithic change in Europe: a high-resolution investigation. In: “Volcanism and Earth’s Atmosphere”, A. Robok and C. Oppenheimer (Eds.). Gephys. Monog. Series, 139, 301-325. Ferguson, J.F., Cogbill, A.H., Warren, R.J. (1994): A geophysical-geological transect of the silent Canyon caldera complex, Pahute Mesa, Nevada. J. Geophys. Res., 99, 4323-4339. Fevola, F., N. Fusi, Mirabile, L. (1993). Rilievi di Sismica Monocanale Ad Alta Risoluzione: Aspetti Dell'evoluzione Geomorfologica del Golfo di Napoli. Ann. Ist. Univ. Nav. Napoli, 60, 61-71. Finetti, I., Morelli, C. (1974): Esplorazione Sismica a Riflessione Dei Golfi di Napoli e Pozzuoli. Boll. Geof. Teor. Appl., 16 (62/63), 175-222. Fisher, R.V., Orsi, G., Ort, M. and Heiken, G. (1993). Mobility of large-volume pyroclastic flow – emplacement of the Campanian Ignimbrite, Italy. J. Volcanol. Geotherm. Res. 56, 205-220. Fusi, N., L. Mirabile, A. Camerlenghi, Ranieri, G. (1991). Marine Geophysical Survey of the Gulf of Napoli (Italy): Relationships Between Submarine Volcanic Activity and Sedimentation. Mem. Soc. Geol. It., 47, 95-114. Garson, M.G., Krs, M. (1976): Geophysical and geological evidence of the relationship of Red Sea transverse tectonics to ancient features. Geol. Soc. Am. Bull., 87, 169-181. Gibson, I. (1967): Preliminary account of a volcanic geology of Fantale, Shoa. Bull. Geophys. Obs. Addis Ababa, 10, 59-67. Gibson, I. (1969): The structure and volcanic geology of an axial portion of the Main Ethiopian Rift. Tectonophysics, 8, 561-565. Ippolito, F., Ortolani, F., Russo, M. (1973): Struttura marginale tirrenica dell’Appennino Campano: reinterpretazione di dati di antiche ricerche di idrocarburi. Mem. Soc. Geol. It. 12, 227, 250. Izzeldin, A.Y. (1989): Transverse structures in the central part of the Red Sea and implications on early stages of oceanic accretion. Geophys. J., 96, 117-129. Johannesson, H., Saemundsson, K. (1998): Geological map of Iceland. Tectonics. Scale 1:500.000. Iceland Institute of Natural History, Reykjavik. Korme, T., Chorowicz, J., Collet, B., Bonaria, F.F. (1997): Volcanic vents rooted on extension fractures and their geodynamic implications in the Ethiopian Rift. J. Volcanol. Geotherm. Res., 79, 205-222. La Croix, A. (1930): Le roches hyperalcalines du massif du Fantale du Col de Balla (Abyssinie). Mem. Soc. Geol. Fr., 6, 89-102. Lagabrielle, Y., Cormier, M.H. (1999): Formation of large summit troughts along the East Pacific Rise as collapse calderas: an evolutionary model. J. Gephys. Res., 104, 12971-12988. Lagabrielle, Y., Garel, E., Dauteuil, O., Cormier, M.H. (2001): Extensional faulting and caldera collapse in the axial region of fast spreading ridges: analogue modelling. J. Gephys. Res., 106, 2005-2015. Le Pichon, X., Francheteau, J. (1978): A plate tectonic analysis of the Red Sea-Gulf of Aden area. Tectonophysics, 46, 369-406. Liotta, D. (1991): The Arbia-Val Marecchia line, Northern Apennines. Ecl. Geol. Helv., 84(2), 413-430. Lipman, P.W. (2000): Calderas. In: “Encyclopedia of volcanoes”, H. Sigurdsson (Ed.). Academic Press, San Francisco, 643-662. Mariani, M., Prato, R., (1988): I bacini neogenici costieri del margine tirrrenico: approccio sismico-stratigrafico. Mem. Soc. Geol. It., 41, 519-531. McKenzie, D.P., Davies, D., Molnar, P. (1970): Plate tectonics of the Red Sea and East Africa. Nature, 226, 243-248. Mohr, P.A. (1962): Surface cauldron subsidence with associated faulting fissure basalt eruption at Gariboldi Pass, Shoa. Bull. Volcanol., 24, 421-428. Mohr, P.A. (1967): Major volcano-tectonic lineament in the Ethiopian Rift System. Narure, 213, 664-665. Mohr, P.A. (1987): Patterns of faulting in the Ethiopian Rift Valley. Tectonophysics, 143, 169-179. Mohr, P.A., Wood, C.A. (1976): Volcano spacing and lithospheric attenuation in the Eastern Rift of Africa. Earth Planet. Sci. Lett., 33, 126-144. Moore, I., Kokelaar, P. (1997): Tectonic influences in piecemeal caldera collapse at Glencoe volcano, Scotland. J. Gol. Soc. London, 154, 765-768. Moore, I., Kokelaar, P. (1998): Tectonically controlled piecemeal caldera collapse: a case study of Glencoe volcano, Scotland. Geol. Soc. Am. Bull., 110, 1448-1466. Newhall, C.G., Dzurisin, D. (1988): Historical unrest at large calderas of the world. U.S. Geological Survey, 1109 pp. Orsi, G., Civetta, L., Del Gaudio, C., de Vita, S., Di Vito, M. A., Isaia, R., Petrazzuoli, S., Ricciardi, G., Ricco, C. (1999). Short-Term Ground Deformations and Seismicity in the Nested Campi Flegrei Caldera (Italy): an example of active block resurgence in a densely populated area. J. Volcanol. Geotherm. Res., 91, 415-451. Orsi, G., Civetta, L., D'Antonio, M., Di Girolamo, P. and Piochi, M. (1995): Step-filling and development of a zoned magma chamber: The Neapolitan Yellow Tuff case history. J. Volcanol. Geotherm. Res., 67, 291-312. Orsi, G., D'Antonio, M., de Vita S. and Gallo G. (1992). The Neapolitan Yellow Tuff, a large-magnitude trachytic phreatoplinian eruption: eruptive dynamics, magma withdrawal and caldera collapse. J. Volcanol. Geotherm. Res., 53, 275-287. Orsi, G., de Vita, S., Di Vito, M.A. (1996): The restless resurgent Campi Flegrei nested caldera (Italy): constraints on its evolution and configuration. J. Volcanol. Geotherm. Res., 74, 179-214. Orsi, G., de Vita, S., Di Vito, M.A., Isaia, R., Nave, R., Heiken, G. (2003): Facing volcanic and related hazards in the Neapolitan area. In: “Earth science in the city: a reader”. G. Heiken et al. Eds., American Geophysical Union, 121-170. Orsi, G., Gallo, G., Zanchi, A. (1991). Simple-shearing block resurgence in caldera depression. A model from Pantelleria and Ischia. J. Volcanol. Geotherm. Res., 47, 1-11. Ortolani, F., Pagliuca, S. (1987): Relationships between volcanism and structures in Campania during the Quaternary. In: “The volcanisclastic rocks of Campania (Southern Italy)”, P. Di Girolamo (Ed.). Rend. Acc. Sc. Fis. Mat. Napoli. Sp. Is., 215-231. Pappalardo, L., Civetta, L., D’Antonio, M., Deino, A., Di Vito, M. A., Orsi, G., Carandente, A., de Vita, S., Isaia, R., Piochi, M. (1999): Chemical and isotopical evolution of the Phlegraean magmatic system before the Campanian Ignimbrite (37 ka) and the Neapolitan Yellow Tuff (12 ka) eruptions. J. Volcanol. Geotherm. Res., 91, 141-166. Peccerillo, A., Yirgu, G., Ayalew, D. (1995): Genesis of acid volcanics along the Main Ethiopian Rift: a case history of Gedemsa volcano. SINET, Ethiopian J. Sci., 18, 23-50. Pescatore, T., G. Diplomatico, M. R. Senatore,M. Tramutoli, Mirabile, L. (1984): Contributi allo Studio del Golfo di Pozzuoli: Aspetti Stratigrafici e Strutturali. Mem. Soc. Geol. It., 27, 133-149. Rohleder, H.P.T., Hitchen, C.S. (1930): Vulkanologiesche Beobachtungen Langs der Bahnlinie Addis Ababa-Djibouti (Abessinien) Z. Vulkan., 12. Self, S., Goff, F., Gardner, J.N., Wright, J.V., Kite, W.M. (1986): Explosive rhyolitic volcanism in the Jemez mountains: vent locations, caldera development and relation to regional structure. Jour. Geophys. Res., 91, 1778-1798. Simkin, T., Howard, K.A. (1970): Caldera collapse in the Galapagos islands. Science, 169, 429-437. Smith, R.L., Bailey, R.A. (1968): Resurgent cauldrons. Mem. Geol. Soc. Am., 116, 613-662. Thrall, R. (1973): Gedemsa caldera, Ethiopia. Center for Astrophysics U.S.A., Reprint Ser. No. 280, 71-80. Vezzoli, L. (1988): Island of Ischia. CNR Quaderni de “La ricerca scientifica” 114 (10), 122 pp. Williams, H. (1941): Calderas and their origin. Bull.Dep. Geol. Sci. University of California publications, 25, 239-246. Wilson, C.J.N., Rogan, A.M., Smith, I.E.M. (1984): Calderas of the Taupo volcanic zone, New Zealand. J. Geophys. Res., 89, 8463-8484. Woldegabriel, G., Walter, R.C., Hart, W., Mertzman, S.A., Aronson, J.L. (1999): Temporal relations and geochemical features of felsic volcanism in the central sector of the Main Ethiopian Rift. Acta Vulcanol., 11, 53-68. | en |
| dc.description.obiettivoSpecifico | 3.5. Geologia e storia dei vulcani ed evoluzione dei magmi | en |
| dc.description.journalType | N/A or not JCR | en |
| dc.description.fulltext | restricted | en |
| dc.contributor.author | De Vita, S. | en |
| dc.contributor.author | Orsi, G. | en |
| dc.contributor.author | Di Vito, M. A. | en |
| dc.contributor.author | Marotta, E. | en |
| dc.contributor.author | Sansivero, F. | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| item.openairetype | article | - |
| item.cerifentitytype | Publications | - |
| item.languageiso639-1 | en | - |
| item.grantfulltext | restricted | - |
| item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
| item.fulltext | With Fulltext | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
| crisitem.author.orcid | 0000-0002-5337-7560 | - |
| crisitem.author.orcid | 0000-0002-7913-9149 | - |
| crisitem.author.orcid | 0000-0001-7211-2173 | - |
| crisitem.author.orcid | 0000-0002-9146-4243 | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.classification.parent | 04. Solid Earth | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| Appears in Collections: | Article published / in press | |
Files in This Item:
| File | Description | Size | Format | Existing users please Login |
|---|---|---|---|---|
| De Vita et al - 2005. The role of prexisting tectonc structures...pdf | 5.88 MB | Adobe PDF |
Page view(s) 5
559
checked on Apr 24, 2024
Download(s)
27
checked on Apr 24, 2024
