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Just kidding, I hope
Originally posted by muzzy
reply to post by zenius
there was another one later, Mag 3.0 at 7:04pm NZST, 8.78km south west of us, offshore Paekakariki, didn't feel it though.
Mag, Lat, Long, Date/Time UTC, Depth
3.0, 3517168,-40.96479,174.90576, 2011/5/22, 07:04:40, 30
"The detonations will happen at night when things are quieter, in a window from May 10 to 14," he said.
The origins of Earth's magnetic field remain a mystery to scientists
how many tons of TNT is a 3.6ML again?
For Jean Paul Ampuero, assistant professor of seismology at Caltech's Seismological Laboratory who studies earthquake dynamics, the most significant finding was that high- and low-frequency seismic waves can come from different areas of a fault. "The high-frequency seismic waves in the Tohoku earthquake were generated much closer to the coast, away from the area of the slip where we saw low-frequency waves," he says.
Simons says there are two factors controlling this behavior; one is because the largest amount of stress (which is what generates the highest-frequency waves) was found at the edges of the slip, not near the center of where the fault began to break. He compares the finding to what happens when you rip a piece of paper in half. "The highest amounts of stress aren't found where the paper has just ripped, but rather right where the paper has not yet been torn," he explains. "We had previously thought high-frequency energy was an indicator of fault slippage, but it didn't correlate in our models of this event." Equally important is how the fault reacts to these stress concentrations; it appears that only the deeper segments of the fault respond to these stresses by producing high-frequency energy.
For seismologist Hiroo Kanamori, Caltech's Smits Professor of Geophysics, Emeritus, who was in Japan at the time of the earthquake and has been studying the region for many years, the most significant finding was that a large slip occurred near the Japan Trench. While smaller earthquakes have happened in the area, it was believed that the relatively soft material of the seafloor would not support a large amount of stress. "The amount of strain associated with this large displacement is nearly five to 10 times larger than we normally see in large megathrust earthquakes," he notes. "It has been generally thought that rocks near the Japan Trench could not accommodate such a large elastic strain."
The researchers are still unsure why such a large strain was able to accumulate in this area. One possibility is that either the subducting seafloor or the upper plate (or both) have some unusual structures -- such as regions that were formerly underwater mountain ranges on the Pacific Plate -- that have now been consumed by the subduction zone and cause the plates to get stuck and build up stress.
Originally posted by muzzy
Makes me think back to MoorfNZ and AoRaki down in Christchurch, isn't that what they were doing down there a short while prior to the Darfield and Port Hills quakes?
Can you imagine the uproar if this is what actaully triggered the Greendale Fault
Originally posted by muzzy
....
Surely those who thought up this process took possible triggering off a Fault into consideration? Risk Analysis?
And the longer without any 7.0+, the larger it will be
How important is accuracy in a progressive analysis?