{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,10,20]],"date-time":"2026-10-20T22:27:38Z","timestamp":1792535258748,"version":"4.5.0"},"reference-count":11,"publisher":"American Geophysical Union (AGU)","issue":"19","license":[{"start":{"date-parts":[[2009,10,6]],"date-time":"2009-10-06T00:00:00Z","timestamp":1254787200000},"content-version":"vor","delay-in-days":5,"URL":"http:\/\/onlinelibrary.wiley.com\/termsAndConditions#vor"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Geophysical Research Letters"],"published-print":{"date-parts":[[2009,10]]},"abstract":"<jats:p>We image the rupture history of the 2009 L'Aquila (central Italy) earthquake using a nonlinear joint inversion of strong motion and GPS data. This earthquake ruptured a normal fault striking along the Apennines axis and dipping to the SW. The inferred slip distribution is heterogeneous and characterized by a small, shallow slip patch located up\u2010dip from the hypocenter (9.5 km depth) and a large, deeper patch located southeastward. The rupture velocity is larger in the up\u2010dip than in the along\u2010strike direction. This difference can be partially accounted by the crustal structure, which is characterized by a high velocity layer above the hypocenter and a lower velocity below. The latter velocity seems to have affected the along strike propagation since the largest slip patch is located at depths between 9 and 14 km. The imaged slip distribution correlates well with the on\u2010fault aftershock pattern as well as with mapped surface breakages.<\/jats:p>","DOI":"10.1029\/2009gl039795","type":"journal-article","created":{"date-parts":[[2009,10,5]],"date-time":"2009-10-05T20:00:35Z","timestamp":1254772835000},"source":"Crossref","is-referenced-by-count":138,"title":["Rupture history of the 2009 L'Aquila (Italy) earthquake from non\u2010linear joint inversion of strong motion and GPS data"],"prefix":"10.1029","volume":"36","author":[{"given":"A.","family":"Cirella","sequence":"first","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia  Rome Italy"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"A.","family":"Piatanesi","sequence":"additional","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia  Rome Italy"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"M.","family":"Cocco","sequence":"additional","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia  Rome Italy"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"E.","family":"Tinti","sequence":"additional","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia  Rome Italy"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"L.","family":"Scognamiglio","sequence":"additional","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia  Rome Italy"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"A.","family":"Michelini","sequence":"additional","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia  Rome Italy"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"A.","family":"Lomax","sequence":"additional","affiliation":[{"name":"ALomax Scientific  Mouans\u2010Sartoux France"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"E.","family":"Boschi","sequence":"additional","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia  Rome Italy"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"13","published-online":{"date-parts":[[2009,10,6]]},"reference":[{"key":"e_1_2_7_2_1","doi-asserted-by":"publisher","DOI":"10.1029\/2009GL039145"},{"key":"e_1_2_7_3_1","doi-asserted-by":"publisher","DOI":"10.1029\/2009GL039293"},{"key":"e_1_2_7_4_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.tecto.2007.08.009"},{"key":"e_1_2_7_5_1","doi-asserted-by":"publisher","DOI":"10.1029\/2008GL034756"},{"key":"e_1_2_7_6_1","unstructured":"Emergeo Working Group(2009) Rilievi geologici di terreno effettuati nell'area epicentrale della sequenza sismica dell'Aquilano del 6 aprile 2009 report Ist. Naz. di Geofis. e Vulcanol. Rome. (Available athttp:\/\/www.earth-prints.org\/handle\/2122\/5036)."},{"key":"e_1_2_7_7_1","doi-asserted-by":"publisher","DOI":"10.1126\/science.324.5925.322"},{"key":"e_1_2_7_8_1","doi-asserted-by":"publisher","DOI":"10.1029\/1998TC900019"},{"key":"e_1_2_7_9_1","first-page":"257","volume-title":"Quaderni de \u201cLa Ricerca Scientifica,\u201d","author":"Parotto M.","year":"1975"},{"key":"e_1_2_7_10_1","doi-asserted-by":"publisher","DOI":"10.1029\/2006JB004821"},{"key":"e_1_2_7_11_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0074-6142(03)80293-0"},{"key":"e_1_2_7_12_1","doi-asserted-by":"publisher","DOI":"10.1785\/0120040177"}],"container-title":["Geophysical Research Letters"],"original-title":[],"language":"en","link":[{"URL":"https:\/\/api.wiley.com\/onlinelibrary\/tdm\/v1\/articles\/10.1029%2F2009GL039795","content-type":"unspecified","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/pdf\/10.1029\/2009GL039795","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2023,10,31]],"date-time":"2023-10-31T19:33:16Z","timestamp":1698780796000},"score":1,"resource":{"primary":{"URL":"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/10.1029\/2009GL039795"}},"subtitle":[],"short-title":[],"issued":{"date-parts":[[2009,10]]},"references-count":11,"journal-issue":{"issue":"19","published-print":{"date-parts":[[2009,10]]}},"alternative-id":["10.1029\/2009GL039795"],"URL":"https:\/\/doi.org\/10.1029\/2009gl039795","archive":["Portico"],"relation":{},"ISSN":["0094-8276","1944-8007"],"issn-type":[{"value":"0094-8276","type":"print"},{"value":"1944-8007","type":"electronic"}],"subject":[],"published":{"date-parts":[[2009,10]]},"article-number":"2009GL039795"}}