Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7906
DC FieldValueLanguage
dc.contributor.authorallD'Agostino, N.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallD'Anastasio, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallAvallone, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.date.accessioned2012-03-23T08:27:21Zen
dc.date.available2012-03-23T08:27:21Zen
dc.date.issued2010en
dc.identifier.urihttp://hdl.handle.net/2122/7906en
dc.description.abstractThe large increase of continuous gps sites occurred in the recent years in the Central Mediterranean plate boundary zone offers the opportunity to study in detail the present-day kinematics in this actively de- forming plate boundary zone. The amount of available cgps data from scientific and commercial networks in the Italian region currently reaches more than 350 cgps stations, including more than 130 sites from the ring network (http://ring.gm.ingv.it), deployed by the Isti- tuto Nazionale di Geofisica e Vulcanologia with high quality gps monuments and co-located with broad- band or very broad band seismometers. gps ambiguity resolution of such a large amount of data asks for a sin- gle and self-consistent processing method, in order to avoid the need of dividing the whole network in sever- al clusters as many of the scientific gps processing codes request and to maximize the processing time speed. The ambizap gps processing algorithm (Blewitt 2008), used to obtain daily ambiguity-fixed network so- lutions allows for a rapid and multiple reanalysis of large regional networks such the one presented in this work, that is composed by more than 580 gps stations. In this presentation we highlights some of the numer- ous scientific motivations behind this project, ranging from the definition of strain distribution and micro- plate kinematics within the plate boundary, to the geodynamic implications for the evolution of the Cala- brian Arc and Aeolian Islands.en
dc.language.isoEnglishen
dc.publisher.nameFabrizio Serra editoreen
dc.relation.ispartofActa Vulcanologicaen
dc.relation.ispartofseries1-2/22(2010)en
dc.subjectCalabrian Arcen
dc.subjectKinematicsen
dc.subjectGPSen
dc.subjectGeodynamicsen
dc.titlePRESENT-DAY KINEMATICS AND RECENT EVOLUTION OF THE CALABRIAN ARC: THE CONTRIBUTION OF LARGE GPS NETWORK ANALYSISen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber13-16en
dc.subject.INGV04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformationsen
dc.relation.referencesBaccheschi P., Margheriti L. and Steckler M. S. (2007). Seismic ani- sotropy reveals focused mantle flow around the Calabrian slab (Southern Italy). «Geophys. Res. Lett.», 34, L05302, doi:10.1029/2006 GL028899. Calais E., DeMets C. and Nocquet J. M. (2003). Evidence for a post-3.16- Ma change in Nubia-Eurasia-North America plate motions: Earth Planet. Sci. Lett.», 216, 1-2, 81-92, doi:10.1016/S0012-821X(03)00482-5. Cheloni D. (2008). Estimating crustal deformation from geodetic data: with applications to the Messina Straits and Friuli area, Ph.D. thesis, University of Bologna, 300 pp. Chiarabba C., Jovane L. and Di Stefano R. (2005). A new view of Italian seismicity using 20 years of instrumental recordings. «Tectono- physics», 395, 3-4, 251-268. Chiarabba C., De Gori P. amd Speranza F. (2008). The southern Tyrrhenian subduction zone: Deep geometry, magmatism and Plio- Pleistocene evolution. «Earth Planet. Sci. Lett.», 268, 3-4, 408-423, doi:10.1016/j.epsl.2008.01.036. Cifelli F., Mattei M. and Rossetti F. (2007). Tectonic evolution of arcuate mountain belts on top of a retreating subduction slab: The example of the Calabrian Arc. «J. Geophys. Res.», 112, B09101, doi:10.1029/2006 JB004848. D’Agostino N. and Selvaggi G. (2004), Crustal motion along the Eura- sia-Nubia plate boundary in the Calabrian Arc and Sicily and active extension in the Messina Straits from gps measurements. «J. Geo- phys. Res.», 109, B11402, doi:10.1029/2004JB002998. DeMets C., Gordon R. G., Argus D. F. and Stein S. (1990). Current plate motions. «Geophys. J. Int.», 101, 425-478. Dewey J. F., Helman M. L., Turco E., Hutton D. H. W. and Knott S. D. (1989). Kinematics of the western Mediterranean. In: M. P. Coward, D. Dietrich and R. G. Park (eds.), Alpine Tectonics, London («Geo- logical Society Special Pubblications», 45), 265-283. Faccenna C., Becker T. W., Lucente F. P., Jolivet L. and Rosetti R. (2001). History of subduction and back-arc extension in the central Mediter- ranean. «Geophys. J. Int.», 145, 809-820. Ferranti L. et alii (2006). Markers of the last interglacial sea-level high stand along the coast of Italy: Tectonic implications. «Quat. Int.», 145- 146, 30-54, doi:10.1016/j.quaint.2005.07.009. Goes S., Giardini D., Jenny S., Hollenstein C., Kahle H. G. and Geiger H. (2004). A recent tectonic reorganization in the south-central Mediter- ranean. «Earth Planet. Sci. Lett.», 226, 3-4, 335-345, doi:10.1016/j.ep- sl.2004.07.038. Gutscher M. A., Roger J., Baptista M. A., Miranda J. M. and Tinti S. (2006). Source of the 1693 Catania earthquake and tsunami (southern Italy): New evidence from tsunami modeling of a locked subduction fault plane. «Geophys. Res. Lett.», 33, L08309, doi:10.1029/2005 GL025442. Gvirtzman Z. and Nur A. (1999). The formation of Mount Etna as the consequence of slab rollback. «Nature», 401, 782-785. Lucente F. P., Chiarabba C., Cimini G. B. and Giardini D. (1999). Tomo- graphic constraints on the geodynamic evolution of the Italian re- gion. «J. Geophys. Res.», 104, 20, 307-20, 327. Malinverno A. and Ryan W. B. (1986). Extension in the Tyrrhenian Sea and shortening in the Appenines as a result of arc migration driven by sinking of the lithosphere. «Tectonics», 5, 227-245. Mattei M., Cifelli F. and D’Agostino N. (2007). The evolution of the Cal- abrian Arc: Evidence from paleomagnetic and gps observations. «Earth Planet. Sci. Lett.», 263, 3-4, 259-274. Nicolosi I., Speranza F. and Chiappini M. (2006). Ultrafast oceanic spreading of the Marsili Basin, southern Tyrrhenian Sea: Evidence from magnetic anomaly analysis. «Geology», 34, 9, 717-720, doi: 10.1130/G22555.1. Patacca E., Sartori R. and Scandone P. (1990). Tyrrhenian basin and Apennines arcs, Kinematics relations since late tortonian times. Mem. Soc. Geol. It.», 45, 425-451. Pondrelli S., Salimbeni S., Ekström G., Morelli A., Gasperini P. and Van- nucci G. (2006). The Italian cmt dataset from 1977 to the present. «Phys. Earth Planet. Int.», 159, 3-4, 286-303, doi:10.1016/j.pepi.2006. 07.008. Schellart W. P., Freeman J., Stegman D. R., Moresi L. and May D. (2007). Evolution and diversity of subduction zones controlled by slab width. «Nature», 446, 308-311, doi:10.1038/nature05615. Selvaggi G. and Chiarabba C. (1995). Seismicity and P-wave velocity im- age of the southern Tyrrhenian subduction zone. «Geophys. J. Int.», 121, 3, 818-826. Serpelloni E., Anzidei M., Baldi P., Casula G. and Galvani A. (2005). Crustal Velocity and Strain-Rate Fields in Italy and Surrounding Re- gions: New Results From the Analysis of Permanent and Non-Per- manent gps Networks. «Geophys. J. Int.», 161, 861-880, doi:10.1111/ j.1365-246X.2006.06218.x. Shaw B., Ambraseys N. N., England P. C., Floyd M. A., Gorman G. J., Higham T. F. G., Jackson J. A., Nocquet J.-M., Pain C. C. and Piggott M. D. (2008). Eastern Mediterranean tectonics and tsunami hazard inferred from the ad 365 earthquake. «Nature Geoscience», 1, 268- 276, doi:10.1038/ngeo151. Wortel M. J. R. and Spakman W. (2000). Subduction and slab detach- ment in the Mediterranean - Carpathian region. «Science», 290, 1910- 1917.en
dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.journalTypeN/A or not JCRen
dc.description.fulltextrestricteden
dc.relation.issn1121-9114en
dc.relation.eissn1724-0425en
dc.contributor.authorD'Agostino, N.en
dc.contributor.authorD'Anastasio, E.en
dc.contributor.authorAvallone, A.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.orcid0000-0002-0444-6240-
crisitem.author.orcid0000-0003-3043-8604-
crisitem.author.orcid0000-0002-0264-2897-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
Appears in Collections:Article published / in press
Files in This Item:
File Description SizeFormat Existing users please Login
D'AGOSTINO_et_alii_ActaVulcanologica2010.pdfMain article347.89 kBAdobe PDF
Show simple item record

Page view(s)

118
checked on Apr 17, 2024

Download(s)

27
checked on Apr 17, 2024

Google ScholarTM

Check