Colliding rocks inside a fault zone as an earthquake happens may be the main generators of high-frequency vibrations, according to a new study.

Earthquakes produce seismic waves with a range of frequencies, from the long, rolling motions that make skyscrapers sway, to the jerky, high-frequency vibrations that cause tremendous damage to houses and other smaller structures.

The new explanation for the high-frequency vibrations is very different than the traditional one, the researchers say. It could help explain puzzling seismic patterns made by some earthquakes.

It could also help scientists predict which faults are likely to produce the more damaging quakes.

“The way we normally think of earthquakes is that stress builds up on a fault until it eventually fails, the two sides slip against each other, and that slip alone is what causes all the ground motions we observe,” says Victor Tsai, an associate professor in the earth, environmental, and planetary sciences department at Brown University.

“The idea of this paper is to evaluate whether there’s something other than just slip. The basic question is: If you have objects colliding inside the fault zone as it slips, what physics could result from that?”

Earthquake vibration model

Drawing from mathematical models that describe the collisions of rocks during landslides and other debris flows, Tsai and coauthor Greg Hirth developed a model that predicts the potential effects of rock collisions in fault zones.

The model suggests the collisions could indeed be the principal driver of high-frequency earthquake vibrations. Combining the collision model with more traditional frictional slip models offers reasonable explanations for earthquake observations that don’t quite fit the traditional model alone, the researchers say.

For example, the combined model helps explain repeating earthquakes—quakes that happen at the same place in a fault and have nearly identical seismic wave forms. The odd thing about these quakes is that they often have very different magnitudes, yet still produce nearly identical ground motions. That’s difficult to explain by slip alone, but makes more sense with the collision model added, the researchers say.

“If you have two earthquakes in the same fault zone, it’s the same rocks that are banging together—or at least rocks of basically the same size,” Tsai says. “So if collisions are producing these high-frequency vibrations, it’s not surprising that you’d get the same ground motions at those frequencies regardless of the amount of slip that occurs.”

The collision model also may help explain why quakes at more mature fault zones—ones that have had lots of quakes over a long period of time—tend to produce less damage compared to quakes of the same magnitude at more immature faults.

More than fault slips

Over time, repeated quakes tend to grind down the rocks in a fault, making the faults smoother. The collision model predicts that smoother faults with less jagged rocks colliding would produce weaker high-frequency vibrations.

Tsai says he and colleagues need to do more work to fully validate the model, but this initial work suggests the idea has promise. If the model does indeed prove valid, it could help classifying which faults are likely to produce more or less damaging quakes.

“People have made some observations that particular types of faults seem to generate more or less high-frequency motion than others, but it has not been clear why faults fall into one category or the other,” he says.

“What we’re providing is a potential framework for understanding that, and we could potentially generalize this to all faults around the world. Smoother faults with rounded internal structures may generally produce less high-frequency motions, while rougher faults would tend to produce more.”

The research also suggests that some long-held ideas about how earthquakes work might need revising.

“In some sense it might mean that we know less about certain aspects of earthquakes than we thought,” Tsai says. “If fault slip isn’t the whole story, then we need a better understanding of fault zone structure.”

The paper appears in Geophysical Research Letters.  The National Science Foundation supported the work.

Source: Brown University

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