Appearances deceive: supposedly “stable” zone make earthquakes even more powerful

rock materials from an actual fault zone — the site of the well-studied 1999 magnitude 7.6 Chi-Chi earthquake in Taiwan.

“In that experimental work, rock materials from boreholes cutting through two different parts of the fault were studied, and their properties were found to be conceptually different,” says Lapusta. “One of them had so-called velocity-weakening friction properties, characteristic of earthquake-producing fault segments, and the other one had velocity-strengthening friction, the kind that tends to produce stable creeping behavior under tectonic loading. However, these ‘stable’ samples were found to be much more susceptible to dynamic weakening during rapid earthquake-type motions, due to shear heating.”

The release notes that Lapusta and Noda used their modeling techniques to explore the consequences of having two fault segments with such lab-determined fault-property combinations. They found that the ostensibly stable area would indeed occasionally creep, and often stop seismic events, but not always. From time to time, dynamic rupture would penetrate that area in just the right way to activate dynamic weakening, resulting in massive slip. They believe that this is what happened in the Chi-Chi earthquake; indeed, the quake’s largest slip occurred in what was believed to be the “stable” zone.

“We find that the model qualitatively reproduces the behavior of the 2011 magnitude 9.0 Tohoku-Oki earthquake as well, with the largest slip occurring in a place that may have been creeping before the event,” says Lapusta. “All of this suggests that the underlying physical model, although based on lab measurements from a different fault, may be qualitatively valid for the area of the great Tohoku-Oki earthquake, giving us a glimpse into the mechanics and physics of that extraordinary event.”

If creeping segments can participate in large earthquakes, it would mean that much larger events than seismologists currently anticipate in many areas of the world are possible. That means, Lapusta says, that the seismic hazard in those areas may need to be reevaluated.

For example, a creeping segment separates the southern and northern parts of California’s San Andreas Fault.

Seismic hazard assessments assume that this segment would stop an earthquake from propagating from one region to the other, limiting the scope of a San Andreas quake. However, the team’s findings imply that a much larger event may be possible than is now anticipated — one that might involve both the Los Angeles and San Francisco metropolitan areas.

“Lapusta and Noda’s realistic earthquake fault models are critical to our understanding of earthquakes — knowledge that is essential to reducing the potential catastrophic consequences of seismic hazards,” says Ares Rosakis, chair of Caltech’s division of engineering and applied science. “This work beautifully illustrates the way that fundamental, interdisciplinary research in the mechanics of seismology at Caltech is having a positive impact on society.”

Now that they have been proven qualitatively to reproduce the behavior of the Tohoku-Oki quake, the models may be useful for exploring future earthquake scenarios in a given region, “including extreme events,” says Lapusta. Such realistic fault models, she adds, may also be used to study how earthquakes may be affected by additional factors such as man-made disturbances resulting from geothermal energy harvesting and CO2 sequestration. “We plan to further develop the modeling to incorporate realistic fault geometries of specific well-instrumented regions, like Southern California and Japan, to better understand their seismic hazard.”

Funding for this research was provided by the National Science Foundation; the Southern California Earthquake Center; the Gordon and Betty Moore Foundation; and the Ministry of Education, Culture, Sports, Science and Technology in Japan.

— Read more in  Hiroyuki Noda and Nadia Lapusta, “Creeping fault segments can turn from stable to destructive due to dynamic weakening,” Nature (9 January 2013) (doi:10.1038/nature11703)