Item talk:Q245289

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Revision as of 19:50, 20 August 2024 by Sky (talk | contribs) (Created page with "{ "USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Frequency-dependent attenuation of the Hispaniola Island region of the Caribbean Sea", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70003911", "url": "https://pubs.usgs.gov/publication/70003911" }, {...")
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{

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   "name": "Frequency-dependent attenuation of the Hispaniola Island region of the Caribbean Sea",
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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\u2013700 km, we estimate an average frequency-dependent Q(f)=224(\u00b127)f0.64(\u00b10.073) 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(\u00b121)f0.71(\u00b10.11) for direct S waves at local distances, \u2264100 km. The strong attenuation observed on both vertical and horizontal components of motion is consistent with expectations for a tectonically active region.",
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