EARTH-SHAKING QUAKE Pictured is a snapshot from a simulation of the southwest-to-northeast component of the ground motions (largest shown in red) generated by the May 12, 2008, Sichaun quake in central China. Scientists can use the simulation to estimate ground motions that would have been experienced anywhere in the region. Click on the image for the story and video.Chavez
A new supercomputer simulation of the large quake that
struck central China
earlier this month could help researchers estimate the size of the ground
motions experienced in areas that didn’t already have instruments in place to
measure those motions. Knowing where ground motions are strongest can help in
assessing where the worst damage may be, such as remote areas with critical
infrastructure.
The epicenter of the magnitude-7.9 temblor was located about
70 kilometers northwest of Chengdu, says Mario
Chavez, a seismological engineer at the National Autonomous University of
Mexico in Mexico City.
Analyses by the U.S. Geological Survey suggest that a patch of the Longmenshan
fault about 315 kilometers long slipped during the two-minute-long quake, he
reported today in Fort Lauderdale, Fla., during a meeting of the American
Geophysical Union. The rupture progressed from southwest to northeast along the
fault zone.
Using data collected by seismometers throughout the region,
he and his colleagues simulated the ground motions that would have been
produced by the massive quake. At depths of about 19 kilometers, where the
quake began, the two sides of the fault slipped past each other as much as 9
meters. At Earth’s surface, however, slippage measured 1.5 meters or less.
Nevertheless, the quake has killed an estimated 80,000 people and caused more
than $10 billion in damage, Chavez says.
Watch the simulation of the earthquake in Sichuan province:
The energy release appears to have been focused, moving to the lower right in the video. The was almost no energy release along the perpendicular line to that release.
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