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1 Department of Geological
Sciences
University of Texas at El Paso
El Paso, Texas
79968-0555
I have relocated M
4.5 earthquakes occurring between 1912 and
1988 and smaller magnitude earthquakes occurring between 1971 and 1988, when
seismograph stations within central Alaska began to increase, to examine changes
in seismicity preceding the 2002 Denali fault earthquake sequence. I have also
determined focal mechanisms from first-motion analysis and waveform modeling for
many of the M
5.5 events. Limited phase and waveform information
for the 1912 Ms 7.2 earthquake are consistent with rupture
at shallow depth on a right-lateral strike-slip fault, although the limited data
cannot distinguish between a range of possible mechanisms. Most other M
4.5 earthquakes occurring within the region prior to 1989 represent
thrust/reverse faulting or strike-slip faulting adjacent to the Denali fault
system. These results highlight the role thrust faulting plays in the
deformation of the Denali region. Stress analysis shows continuity in the
direction of maximum compressive stress (
1) between
the western Denali fault zone and the Castle Mountain fault/Upper Cook Inlet
region, suggesting the crust is behaving rigidly to transfer compression to the
Denali fault zone and faults located to the north.
This article has been cited by other articles:
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N. A. Ratchkovski, S. Wiemer, and R. A. Hansen Seismotectonics of the Central Denali Fault, Alaska, and the 2002 Denali Fault Earthquake Sequence Bulletin of the Seismological Society of America, December 1, 2004; 94(6B): S156 - S174. [Abstract] [Full Text] [PDF] |
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B. T. Aagaard, G. Anderson, and K. W. Hudnut Dynamic Rupture Modeling of the Transition from Thrust to Strike-Slip Motion in the 2002 Denali Fault Earthquake, Alaska Bulletin of the Seismological Society of America, December 1, 2004; 94(6B): S190 - S201. [Abstract] [Full Text] [PDF] |
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