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GEOREF RECORD

A model for the shape of the Fourier amplitude spectrum of acceleration at high frequencies

John G. Anderson and Susan E. Hough
A model for the shape of the Fourier amplitude spectrum of acceleration at high frequencies
Bulletin of the Seismological Society of America (October 1984) 74 (5): 1969-1993

Abstract

At high frequencies f the spectrum of S-wave accelerations is characterized by a trend of exponential decay, e (super -pi kappa f) . In our study, the spectral decay parameter kappa increases gradually as the epicentral distance increases. For multiple recordings of the San Fernando earthquake, kappa increases slowly with distance, and kappa is smaller for sites on rock than for sites on alluvium. Under the assumption that the Fourier spectrum of acceleration at the source is constant above the corner frequency (an omega (super -2) source model), the exponential decay is consistent with an attenuation model in which Q increases rapidly with depth in the shallow crustal layers.--Modified journal abstract.


ISSN: 0037-1106
EISSN: 1943-3573
Coden: BSSAAP
Serial Title: Bulletin of the Seismological Society of America
Serial Volume: 74
Serial Issue: 5
Title: A model for the shape of the Fourier amplitude spectrum of acceleration at high frequencies
Affiliation: Scripps Inst. Oceanogr., Inst. Geophys. and Planet. Phys., La Jolla, CA, United States
Pages: 1969-1993
Published: 198410
Text Language: English
Publisher: Seismological Society of America, Berkeley, CA, United States
References: 50
Accession Number: 1985-015841
Categories: Engineering geology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 2 tables, sketch maps
N32°40'00" - N33°19'60", W116°00'00" - W115°00'00"
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute.
Update Code: 1985
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