Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/542
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dc.contributor.authorallBattaglia, M.; Seismological Laboratory, University of California, Berkeley, California, USAIstituto Nazionale di Oceanografia e Geofisica Sperimentale, Centro Ricerche Sismologiche, Udine, Italyen
dc.contributor.authorallMurray, M. H.; Seismological Laboratory, University of California, Berkeley, California, USAen
dc.contributor.authorallSerpelloni, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallBurgmann, R.; Department of Earth and Planetary Science, University of California, Berkeley, California, USAen
dc.date.accessioned2005-11-23T11:04:10Zen
dc.date.available2005-11-23T11:04:10Zen
dc.date.issued2004-09en
dc.identifier.urihttp://hdl.handle.net/2122/542en
dc.description.abstract[1] We use GPS measurements and block modeling to investigate the present-day deformation of the Adriatic region, whose kinematics within the Nubia-Eurasia plate boundary zone is not well constrained and remains controversial. Block modeling allows us to compute rigidplate angular velocities while accounting for elastic strain accumulation along block-bounding faults. Results suggest that the Adriatic is a microplate (Adria) and that the southern boundary with the Nubia plate and the Aegean domain may be located along the Apulia Escarpment and the Kefallinia fault. Geodetic data alone cannot discriminate between a single block (AP) or a two blocks (GDAP) description of Adria, but the GDAP model predicts boundary slip rates that are in better agreement with observations from previous studies. INDEX TERMS: 1208 Geodesy and Gravity: Crustal movements—intraplate (8110); 1243 Geodesy and Gravity: Space geodetic surveys; 3210 Mathematical Geophysics: Modeling; 8107 Tectonophysics: Continental neotectonics; 9335 Information Related to Geographic Region: Europe. Citation: Battaglia, M., M. H. Murray, E. Serpelloni, and R. Bu¨rgmann (2004), The Adriatic region: An independent microplate within the Africa-Eurasia collision zone, Geophys. Res. Lett., 31, L09605, doi:10.1029/ 2004GL019723.en
dc.format.extent353470 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofGEOPHYSICAL RESEARCH LETTERS,en
dc.relation.ispartofseries09/31(2004)en
dc.subjectAdriaticen
dc.subjectmicroplateen
dc.titleThe Adriatic region: An independent microplate within the Africa-Eurasia collision zoneen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber(605)en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneousen
dc.identifier.doidoi:10.1029/2004GL019723en
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Lett., 28, 4315–4318. Nocquet, J. M., and E. Calais (2003), Crustal velocity field of western Europe from permanent GPS array solutions, 1996 – 2001, Geophys. J. Int., 154, 72–88. Nocquet, J. M., E. Calais, Z. Altamini, P. Sillard, and C. Boucher (2001), Intraplate deformation in western Europe deduced from an analysis of the International Terrestrial Reference Frame 1997 (ITRF97) velocity field, J. Geophys. Res., 106, 11,239– 11,257. Oldow, J. S., et al. (2002), Active fragmentation of Adria, the north Africa promontory, central Mediterranean orogen, Geology, 30, 779– 782. Pondrelli, S., et al. (2002), European-Mediterranean regional centroid-moment tensors: 1997– 2000, Phys. Earth Planet. Inter., 130, 71–101. Sella, G., T. H. Dixon, and A. Mao (2002), REVEL: A model for recent plate velocities from space geodesy, J. Geophys. Res., 107(B4), 2081, doi:10.1029/2000JB000033. Serpelloni, E., et al. (2001), Geodetic deformations in the central-southern Apennines (Italy) from repeated GPS surveys, Ann. Geofis., 44, 627– 647. Serpelloni, E., et al. (2002), Combination of permanent and non-permanent GPS networks for the evaluation of the strain-rate field in the central Mediterranean area, Boll. Geof. Teor. Appl., 43, 195– 219. Thatcher, W. (2003), GPS constraints on the kinematics of continental deformation, Int. Geol. Rev., 45, 191–212. Van Dijk, J. P., and P. J. J. Scheepers (1995), Neotectonic rotations in the Calabrian Arc: Implications for a Pliocene-Recent geodynamic scenario for the central Mediterranean, Earth Sci. Rev., 39, 207– 246. Ward, S. N. (1994), Constraints on the seismo-tectonics of the central Mediterranean from very long baseline interferometry, Geophys. J. Int., 117, 441– 452. Wortmann, U. G., H. Weissert, H. Funk, and J. Hauck (2001), Alpine plate kinematics revisited: The Adria problem, Tectonics, 20, 134–147.en
dc.description.fulltextreserveden
dc.contributor.authorBattaglia, M.en
dc.contributor.authorMurray, M. H.en
dc.contributor.authorSerpelloni, E.en
dc.contributor.authorBurgmann, R.en
dc.contributor.departmentSeismological Laboratory, University of California, Berkeley, California, USAIstituto Nazionale di Oceanografia e Geofisica Sperimentale, Centro Ricerche Sismologiche, Udine, Italyen
dc.contributor.departmentSeismological Laboratory, University of California, Berkeley, California, USAen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentDepartment of Earth and Planetary Science, University of California, Berkeley, California, USAen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversity of Rome “La Sapienza,” Department of Earth Sciences, Rome, Italy-
crisitem.author.deptSeismological Laboratory, University of California, Berkeley, California, USA-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptUniversity of California, Berkeley, CA, United States-
crisitem.author.orcid0000-0003-4726-5287-
crisitem.author.orcid0000-0003-1822-403X-
crisitem.author.orcid0000-0002-3560-044X-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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