دورية أكاديمية
Forearc extension and slow rollback of the Calabrian Arc from GPS measurements
| العنوان: | Forearc extension and slow rollback of the Calabrian Arc from GPS measurements |
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| المؤلفون: | D'Agostino, N., D'Anastasio, E., Gervasi, A., Guerra, I., Nedimovic, M. R., Seeber, L., Steckler, M. |
| المساهمون: | D'Agostino, N., Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italia, D'Anastasio, E., Gervasi, A., Guerra, I., Dipartimento di Fisica, Università della Calabria, Nedimovic, M. R., Department of Earth Sciences, Dalhousie University, Halifax, Nova Scotia, Canada., Seeber, L., Lamont-Doherty Earth Observatory, The Earth Institute at Columbia University, Palisades, New York, USA., Steckler, M., Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia |
| بيانات النشر: | American Geophysical Union |
| سنة النشر: | 2011 |
| المجموعة: | Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) |
| مصطلحات موضوعية: | Calabrian Arc, GPS, 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations |
| الوصف: | Here we describe the horizontal velocities of continuous GPS stations in the Calabrian Arc (CA) and surrounding regions. The appropriate reference frame to evaluate the crustal motion of the CA is considered by assessing the internal deformation and the relative motion of the crustal blocks in the foreland of the Apennines␣Ionian␣Maghrebides subduction system. We propose that the motion of CA rela- tive to the subducting Ionian lower plate is most properly assessed by minimizing the GPS velocities in Apulia. In this reference frame the significant ␣2 mm/yr southeast- ward motion of the stations on the Ionian flank of the CA shows that the arc is still moving towards the trench in agreement with the observations of active shortening in the Ioanian wedge. This southeastward migration is associated to 1.4 ± 0.3 mm/yr E␣W extension of the forearc in northern Calabria, comparable with the seismic strain averaged in the last 500 years. The limited subaerial exposure decreases the resolution on locking of the subduction interface but the distribution and direction of crustal extension along the CA impose important constraints on geodynamic interpreta- tions of the area. ; Published ; L17304 ; 3.2. Tettonica attiva ; JCR Journal ; reserved |
| نوع الوثيقة: | article in journal/newspaper |
| اللغة: | English |
| العلاقة: | Geophysical Research Letters; /38 (2011); http://hdl.handle.net/2122/7100Test; http://www.agu.org/journals/gl/gl1117/2011GL048270Test/ |
| DOI: | 10.1029/2011GL048270 |
| الإتاحة: | https://doi.org/10.1029/2011GL048270Test http://hdl.handle.net/2122/7100Test http://www.agu.org/journals/gl/gl1117/2011GL048270Test/ |
| حقوق: | restricted |
| رقم الانضمام: | edsbas.8B554600 |
| قاعدة البيانات: | BASE |
| DOI: | 10.1029/2011GL048270 |
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