Recurrent Intraplate Tectonism in the New Madrid Seismic Zone

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 caus...

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Veröffentlicht in:Science (American Association for the Advancement of Science) 1980-08, Vol.209 (4460), p.971-976
Hauptverfasser: Zoback, M. D., Hamilton, R. M., Crone, A. J., Russ, D. P., McKeown, F. A., Brockman, S. R.
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container_end_page 976
container_issue 4460
container_start_page 971
container_title Science (American Association for the Advancement of Science)
container_volume 209
creator Zoback, M. D.
Hamilton, R. M.
Crone, A. J.
Russ, D. P.
McKeown, F. A.
Brockman, S. R.
description 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.
doi_str_mv 10.1126/science.209.4460.971
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identifier ISSN: 0036-8075
ispartof Science (American Association for the Advancement of Science), 1980-08, Vol.209 (4460), p.971-976
issn 0036-8075
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language eng
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source Jstor Complete Legacy; Science Online_科学在线
subjects EARTHQUAKES
Fault lines
Fault zones
GEOLOGIC FAULTS
GEOLOGIC STRUCTURES
Geology
GEOSCIENCES
Groves
IGNEOUS ROCKS
INTRUSION
MIDWEST REGION
Missouri
NORTH AMERICA
Plate tectonics
PLUTONIC ROCKS
Plutons
Reflectors
RIFT ZONES
RISK ASSESSMENT
ROCKS
Sediments
SEISMIC EVENTS
SEISMICITY
Seismological research
TECTONICS
USA 580201 -- Geophysics-- Seismology & Tectonics-- (1980-1989)
title Recurrent Intraplate Tectonism in the New Madrid Seismic Zone
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