Seismic properties and processes along the Subduction Plate Interface: the Februrary 2010 Mw 8.8 Maule, Chile Earthquake

Hicks, Stephen
Seismic properties and processes along the Subduction Plate Interface: the Februrary 2010 Mw 8.8 Maule, Chile Earthquake. PhD thesis, University of Liverpool.

[img] Text
Hicks_ThesisMauleCorrectedNov15.pdf - Unspecified
Access to this file is embargoed until Unspecified.
Available under License Creative Commons Attribution.

Download (11MB)
[img] Text
HicksSte_Aug2015_2036999.pdf - Unspecified
Available under License Creative Commons Attribution.

Download (11MB)


The seismogenic zone of subduction margins has the potential to generate some of the world’s largest earthquakes. A detailed study of the 2010 Mw 8.8 Maule, Chile rupture has enabled interpretation of the controls that govern subduction zone seismic behaviour across the earthquake cycle. In this thesis, we focus on two aspects of the central Chile margin: (1) imaging physical properties in the forearc and along the plate interface; (2) assessing source complexity of megathrust ruptures. We exploit a dataset of seismic body wave onset times from local aftershocks recorded on a temporary network to derive a 3-D seismic velocity model of the Maule rupture area. We image the main domains of the subduction zone and find a high velocity anomaly located along the plate interface, which we initially interpret as a subducted topographic high. We then develop a second, more accurate velocity model that uses an improved arrival time dataset together with observations from ocean-bottom seismometers. This refined model gives a sharper view of both the plate interface close to the trench, and the marine forearc. We show that ancient blocks of dense mantle in the lower forearc may have decelerated slip during the Maule earthquake and contributed to its nucleation. Furthermore, we infer that fluid saturated sediments inhibited significant slip close to the trench. We study source processes of a large aftershock of the Maule sequence, the 2011 Mw 7.1 Araucania earthquake, by inverting local seismic waveforms for a multiple point-source faulting solution. We find this earthquake constituted rupture on the plate interface followed by almost instantaneous slip along a normal fault in the overriding plate: the first observation of its kind. The second rupture of this closely-spaced doublet was hidden from teleseismic faulting solutions, and may have been dynamically triggered by S-waves from the first event. Overall, our work highlights the role played by the upper plate in subduction zone seismogenesis. We suggest that seismic velocities can help to characterise the behaviour of future large megathrust earthquakes. We show that the potential hazard posed by closely-spaced doublets involving the upper plate should be accounted for in real-time tsunami warning systems by using local waveform analysis.

Item Type: Thesis (PhD)
Additional Information: Date: 2015-08 (completed)
Uncontrolled Keywords: Seismology, tectonophysics, subduction zone, faulting, faults, earthquake, earthquake seismology, tomography, moment tensor
Subjects: ?? Q1 ??
?? QC ??
?? QE ??
Depositing User: Symplectic Admin
Date Deposited: 18 Jan 2016 11:14
Last Modified: 17 Dec 2022 01:31
DOI: 10.17638/02036999