Seismic-Wave Attenuation Associated with Crustal Faults in the New Madrid Seismic Zone

The attenuation of upper crustal seismic waves that are refracted with a velocity of about 6 kilometers per second varies greatly among profiles in the area of the New Madrid seismic zone in the central Mississippi Valley. The waves that have the strongest attenuation pass through the seismic trend...

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Bibliographic Details
Published in:Science (American Association for the Advancement of Science) 1990-04, Vol.248 (4953), p.351-354
Main Authors: Hamilton, R. M., Mooney, W. D.
Format: Article
Language:English
Subjects:
Arkansas
Carbonate rocks
Curvature
Earthquake prediction
Earthquakes
Fault zones
Kentucky
Missouri
Natural disasters
Seismic waves
Shales
Surfactants
Tennessee
Transcriptional regulatory elements
Wave attenuation
Wave velocity
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Summary:The attenuation of upper crustal seismic waves that are refracted with a velocity of about 6 kilometers per second varies greatly among profiles in the area of the New Madrid seismic zone in the central Mississippi Valley. The waves that have the strongest attenuation pass through the seismic trend along the axis of the Reelfoot rift in the area of the Blytheville arch. Defocusing of the waves in a low-velocity zone and/or seismic scattering and absorption could cause the attenuation; these effects are most likely associated with the highly deformed rocks along the arch. Consequently, strong seismic-wave attenuation may be a useful criterion for identifying seismogenic fault zones.
ISSN:0036-8075
1095-9203
DOI:10.1126/science.248.4953.351