Local Earthquake Tomography of Central Costa Rica: Transition from seamount to ridge subduction.

Dinc-Akdogan, Nilay, Koulakov, I., Thorwart, Martin, Rabbel, Wolfgang, Flueh, Ernst R., Arroyo, Ivonne Gabriela, Taylor, W. and Alvarado, G. (2010) Local Earthquake Tomography of Central Costa Rica: Transition from seamount to ridge subduction. Open Access Geophysical Journal International, 183 (1). pp. 286-302. DOI 10.1111/j.1365-246X.2010.04717.x.

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The structure and seismicity of the subduction zone of centralCosta Rica have been investigated
with local earthquake tomography down to ca. 50 km depth. Seismic traveltime data sets of
three on- and offshore seismic networks were combined for a simultaneous inversion of
hypocentre locations, 3-D structure of P-wave velocity and Vp/Vs ratio using about 2000 highquality
events. The seismicity and slab geometry as well as Vp and Vp/Vs show significant
lateral variation along the subduction zone corresponding to the changes of the incoming plate
which consists of serpentinized oceanic lithosphere in the northwest, a seamount province
in the centre and the subducting Cocos Ridge in the southeast of the investigation area.
Three prominent features can be identified in the Vp and Vp/Vs tomograms: a high-velocity
zone with a perturbation of 4–10 per cent representing the subducting slab, a low-velocity
zone (10–20 per cent) in the forearc crust probably caused by deformation, fluid release and
hydration and a low-velocity zone below the volcanic arc related to upwelling fluids and
magma. Unlike previously suggested, the dip of the subducting slab does not decrease to the
south. Instead, an average steepening of the plate interface from 30◦ to 45◦ is observed from
north to south and a transition from a plane to a step-shaped plate interface. This is connected
with a change in the deformation style of the overriding plate where roughly planar, partly
conjugated, clusters of seismicity of regionally varying dip are observed. It can be shown that
the central Costa Rica Deformation Belt represents a deep crustal transition zone extending
from the surface down to 40 km depth. This transition zone indicates the lateral termination
of the active part of the volcanic chain and seems to be related to the changing structure of the
incoming plate as well.

Document Type: Article
Additional Information: This article has been published in Geophysical Journal International ©2010 The Authors Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved.
Keywords: Seismology; Geophysics; Earth quakes; Central Costa Rica; subduction zone processes; seismicity and tectonics; seismic tomography
Research affiliation: OceanRep > SFB 574
OceanRep > SFB 574 > A2
OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-GDY Marine Geodynamics
Kiel University
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1111/j.1365-246X.2010.04717.x
ISSN: 0956-540X
Projects: Future Ocean
Contribution Number:
SFB 574120
Date Deposited: 13 Jul 2010 09:40
Last Modified: 10 Jul 2018 12:58
URI: http://oceanrep.geomar.de/id/eprint/8613

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