The 1998 Aiquile, Bolivia earthquake: A seismically active fault revealed with InSAR

Using SAR interferometry (InSAR), the deformation field of the Mw=6.6, 1998 Aiquile, Bolivia earthquake is mapped, and the epicentre accurately located for the first time. Elastic dislocation modelling is used to demonstrate that the measured displacements are best explained with a ∼N-S oriented fau...

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Main Authors: Funning, G, Barke, R, Lamb, S, Minaya, E, Parsons, B, Wright, T
Format: Journal article
Language:English
Published: 2005
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author Funning, G
Barke, R
Lamb, S
Minaya, E
Parsons, B
Wright, T
author_facet Funning, G
Barke, R
Lamb, S
Minaya, E
Parsons, B
Wright, T
author_sort Funning, G
collection OXFORD
description Using SAR interferometry (InSAR), the deformation field of the Mw=6.6, 1998 Aiquile, Bolivia earthquake is mapped, and the epicentre accurately located for the first time. Elastic dislocation modelling is used to demonstrate that the measured displacements are best explained with a ∼N-S oriented fault, with a strike that is oblique to the principal topographic features in the region, and a location that agrees with a Modified Mercalli Intensity map constructed from observations of damage in the surrounding area. A variable-slip solution for a fault in this orientation is obtained which predicts peak slip of 1.42 m at depths of ∼4-5 km on the fault plane and has an estimated seismic moment, M0=8.44×1018 N m, which agrees with estimates from long-period seismology. This is the first time that a fault has been demonstrated unambiguously to be active in the Central Andes, and since there was no previous knowledge of an active fault with this location or orientation, a necessary conclusion is that our understanding of seismic hazard in this region is limited. © 2005 Elsevier B.V. All rights reserved.
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spelling oxford-uuid:c6e6c783-e2c7-4946-9d36-8e9f2fb9a4ac2022-03-27T06:41:10ZThe 1998 Aiquile, Bolivia earthquake: A seismically active fault revealed with InSARJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:c6e6c783-e2c7-4946-9d36-8e9f2fb9a4acEnglishSymplectic Elements at Oxford2005Funning, GBarke, RLamb, SMinaya, EParsons, BWright, TUsing SAR interferometry (InSAR), the deformation field of the Mw=6.6, 1998 Aiquile, Bolivia earthquake is mapped, and the epicentre accurately located for the first time. Elastic dislocation modelling is used to demonstrate that the measured displacements are best explained with a ∼N-S oriented fault, with a strike that is oblique to the principal topographic features in the region, and a location that agrees with a Modified Mercalli Intensity map constructed from observations of damage in the surrounding area. A variable-slip solution for a fault in this orientation is obtained which predicts peak slip of 1.42 m at depths of ∼4-5 km on the fault plane and has an estimated seismic moment, M0=8.44×1018 N m, which agrees with estimates from long-period seismology. This is the first time that a fault has been demonstrated unambiguously to be active in the Central Andes, and since there was no previous knowledge of an active fault with this location or orientation, a necessary conclusion is that our understanding of seismic hazard in this region is limited. © 2005 Elsevier B.V. All rights reserved.
spellingShingle Funning, G
Barke, R
Lamb, S
Minaya, E
Parsons, B
Wright, T
The 1998 Aiquile, Bolivia earthquake: A seismically active fault revealed with InSAR
title The 1998 Aiquile, Bolivia earthquake: A seismically active fault revealed with InSAR
title_full The 1998 Aiquile, Bolivia earthquake: A seismically active fault revealed with InSAR
title_fullStr The 1998 Aiquile, Bolivia earthquake: A seismically active fault revealed with InSAR
title_full_unstemmed The 1998 Aiquile, Bolivia earthquake: A seismically active fault revealed with InSAR
title_short The 1998 Aiquile, Bolivia earthquake: A seismically active fault revealed with InSAR
title_sort 1998 aiquile bolivia earthquake a seismically active fault revealed with insar
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