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Science 29 August 1980: Vol. 209. no. 4460, pp. 971 - 976 DOI: 10.1126/science.209.4460.971
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Articles
Recurrent Intraplate Tectonism in the New Madrid Seismic Zone
M. D. Zoback 1,
R. M. Hamilton 1,
A. J. Crone 2,
D. P. Russ 2,
F. A. McKeown 2, and
S. R. Brockman 2
1 U.S. Geological Survey (USGS) National Center, Reston, Virginia 22092
2 USGS Federal Center, Denver, Colorado 80225
For the first time, New Madrid seismicity can be linked to specific structural features that have been reactivated through geologic time. Extensive seismic reflection profiling reveals major faults coincident with the main earthquake trends in the area and with structural deformation apparently caused by repeated episodes of igneous activity.
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- An integrated study of crustal structure and regional wave propagation for southeastern Missouri.
- C. A. Langston (1994)
Bulletin of the Seismological Society of America
84, 105-118
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- Rapid Intraplate Strain Accumulation in the New Madrid Seismic Zone.
- L. Liu, L. Liu, M. D. Zoback, and P. Segall (1992)
Science
257, 1666-1669
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- Seismic-Wave Attenuation Associated with Crustal Faults in the New Madrid Seismic Zone.
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248, 351-354
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- Mini-sosie high-resolution reflection survey of the Cottonwood Grove fault in northwestern Tennessee.
- J. L. SEXTON and P. B. JONES (1988)
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- Intraplate seismicity induced by stress concentration at crustal heterogeneities--the Hohenzollern Graben, a case history.
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- Evidence for contemporary vertical fault displacement from precise leveling data near the New Madrid seismic zone, western Kentucky.
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213, 96-104
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