Frequency-dependent attenuation of the Hispaniola Island region of the Caribbean Sea

Bulletin of the Seismological Society of America
By: , and 

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Abstract

We determine frequency-dependent attenuation 1/Q(f) for the Hispaniola region using direct S and Lg waves over five distinct passbands from 0.5 to 16 Hz. Data consist of 832 high-quality vertical and horizontal component waveforms recorded on short-period and broadband seismometers from the devastating 12 January 2010 M 7.0 Haiti earthquake and the rich sequence of aftershocks. For the distance range 250–700 km, we estimate an average frequency-dependent Q(f)=224(±27)f0.64(±0.073) using horizontal components of motion and note that Q(f) estimated with Lg at regional distances is very consistent across vertical and horizontal components. We also determine a Q(f)=142(±21)f0.71(±0.11) for direct S waves at local distances, ≤100 km. The strong attenuation observed on both vertical and horizontal components of motion is consistent with expectations for a tectonically active region.
Publication type Article
Publication Subtype Journal Article
Title Frequency-dependent attenuation of the Hispaniola Island region of the Caribbean Sea
Series title Bulletin of the Seismological Society of America
DOI 10.1785/0120110137
Volume 102
Issue 2
Year Published 2012
Language English
Publisher Seismological Society of America
Publisher location El Cerrito, CA
Contributing office(s) Geologic Hazards Science Center
Description 10 p.
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Bulletin of the Seismological Society of America
First page 773
Last page 782
Other Geospatial Caribbean Sea;Hispaniola
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