Deep structure and tectonics of the northern‐central Apennines as seen by regional‐scale tomography and 3‐D located earthquakes. Issue 10 (10th October 2013)

• Record Type: Journal Article
• Authors: Carannante, S.; Monachesi, G.; Cattaneo, M.; Amato, A.; Chiarabba, C.
• Is Part Of: Journal of geophysical research. Volume 118:Issue 10(2013:Oct.)
• Page Start: 5391
• Page End: 5403
• Publication Date: 2013-10-10
• Subjects: Geomagnetism -- Periodicals; Geochemistry -- Periodicals; Geophysics -- Periodicals; Earth sciences -- Periodicals; 551.1
• DOI: 10.1002/jgrb.50371
• Languages: English
• ISSNs: 2169-9313

Abstract

<abstract abstract-type="main"> <title>Abstract</title> <p>[1] In this study we present new high‐resolution, regional‐scale, <italic>Vp</italic> and <italic>Vp</italic>/<italic>Vs</italic> models of the northern‐central Apennines along with accurate 3‐D locations of a large set of local earthquakes. The main velocity anomalies are consistent with the surface geology in the shallow layers and present evidence for fluids stored within the basement at greater depths beneath the extensional belt. The Adria and Tyrrhenian mantle are defined by positive velocity anomalies below 30 km depth, while a low‐<italic>Vp</italic>, high‐<italic>Vp</italic>/<italic>Vs</italic> region in between indicates the existence of a hydrated wedge. The results yield new constraints on active processes in the Apennines and more generally envisage the evolution of a postcollisional belt. Velocity anomalies and earthquakes are consistent with a complex system of delamination and sinking of the Adria continental lithosphere, with the peeling of the crust identified by intermediate‐depth seismicity. Change of seismicity and structural patterns along the belt indicates that this tectonic process is diachronous and that fluids, released by sunken lithosphere, are stored within the crust, conditioning the occurrence of seismicity and the onset of extension.</p> </abstract>