EMBARGOED BY SCIENCE FOR RELEASE: 11 A.M., U.S. PACIFIC DAYLIGHT TIME, JULY 10, 2014
As scientists learn more about earthquakes that rupture at fault zones near the planet’s surface—and the mechanisms that trigger them—an even more intriguing earthquake mystery lies deeper in the planet.
Scientists at Scripps Institution of Oceanography at UC San Diego have discovered the first evidence that deep earthquakes, those breaking at more than 400 kilometers (250 miles) below Earth’s surface, can rupture much faster than ordinary earthquakes. The finding gives seismologists new clues about the forces behind deep earthquakes as well as fast-breaking earthquakes that strike near the surface.
Seismologists have documented a handful of these events, in which an earthquake’s rupture travels faster than the shear waves of seismic energy that it radiates. These “supershear” earthquakes have rupture speeds of four kilometers per second (an astonishing 9,000 miles per hour) or more.
In a National Science Foundation-funded study reported in the June 11, 2014, issue of the journal Science, Scripps geophysicists Zhongwen Zhan and Peter Shearer of Scripps, along with their colleagues at Caltech, discovered the first deep supershear earthquake while examining the aftershocks of a magnitude 8.3 earthquake on May 24, 2013, in the Sea of Okhotsk off the Russian mainland.
Details of a magnitude 6.7 aftershock of the event captured Zhan’s attention. Analyzing data from the IRIS (Incorporated Research Institutions for Seismology) consortium, which coordinates a global network of seismological instruments, Zhan noted that most seismometers around the world yielded similar records, all suggesting an anomalously short duration for a magnitude 6.7 earthquake.
Data from one seismometer, however, stationed closest to the event in Russia’s Kamchatka Peninsula, told a different story with intriguing details.
After closely analyzing the data, Zhan not only found that the aftershock ruptured extremely deeply at 640 kilometers (400 miles) below the earth’s surface, but its rupture velocity was extraordinary—about eight kilometers per second (five miles per second), nearly 50 percent faster than the shear wave velocity at that depth.
“For a 6.7 earthquake you would expect a duration of seven to eight seconds, but this one lasted just two seconds,” said Shearer, a geophysics professor in the Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics (IGPP) at Scripps. “This is the first definitive example of supershear rupture for a deep earthquake since previously supershear ruptures have been documented only for shallow earthquakes.”
“This finding will help us understand why deep earthquakes happen,” said Zhan. “One quarter of earthquakes occur at large depths, and some of these can be pretty big, but we still don’t understand why they happen. So this earthquake provides a new observation for deep earthquakes and high-rupture speeds.”
Zhan also believes the new information will be useful in examining ultra-fast earthquakes and their potential for impacting fault zones near the earth’s surface. Although not of supershear caliber, California’s destructive 1994 Northridge earthquake had a comparable size and geometry to that of the 6.7 Sea of Okhotsk aftershock.
“If a shallow earthquake such as Northridge goes supershear, it could cause even more shaking and possibly more damage,” said Zhan.
Coauthors of the paper include Donald Helmberger and Hiroo Kanamori of Caltech.
Note: Project IDA, based at Scripps-IGPP, operates nearly a third of IRIS’s Global Seismographic Network.
Related Image Gallery: Super-fast Deep Earthquake