The recent 8.2-magnitude earthquake in Iquique, Chile, did not relieve all the stress on the fault, and researchers say that means another quake is possible.
The quake occurred in a gap on a fault line that’s held since 1877.
“We assumed that the area of the 1877 earthquake would eventually rupture, but all indications are that this 8.2 event was not the 8.8 event we were looking for,” says Kevin P. Furlong, professor of geophysics at Penn State. “We looked at it to see if this was the big one.”
Seismologists expect that areas of faults will react the same way over and over. However, the April 2014 earthquake was about nine times less energetic than the one in 1877 and was incapable of releasing all the stress on the fault, leaving open the possibility of another earthquake.
The Iquique earthquake took place on the northern portion of the subduction zone formed when the Nazca tectonic plate slides under the South American plate. This is one of the longest uninterrupted plate boundaries on the planet and the site of many earthquakes and volcanos.
The 8.2 earthquake was foreshadowed by a systematic sequence of foreshocks recorded at 6.0, 6.5, 6.7, and 6.2, with each foreshock triggering the next until the main earthquake occurred.
These earthquakes relieved the stresses on some parts of the fault. Then the 8.2 earthquake relieved more stress, followed by a series of aftershocks in the range of 7.7. While the aftershocks did fill in some of the gaps left by the 8.2 earthquake, the large earthquake and aftershocks could not fill in the entire gap where the fault had not ruptured in a very long time. That area is unruptured and still under stress.
The foreshocks eased some of the built up stress on 60 to 100 miles of fault, and the main shock released stress on about 155 miles, but about 155 miles of fault remain unchanged, the researchers report in Nature.
“There can still be a big earthquake there,” says Furlong. “It didn’t release the total hazard, but it told us something about this large earthquake area. That an 8.8 rupture doesn’t always happen.”
The researchers were able to do this analysis in near real time because of the availability of large computing power and previously laid groundwork.
The computing power allowed researchers to model the fault more accurately. In the past, subduction zones were modeled as if they were on a plane, but the plate that is subducting curves underneath the other plate creating a 3-dimensional fault line. The researchers used a model that accounted for this curving and so more accurately recreated the stresses on the real geology at the fault.
“One of the things the US Geological Survey (USGS) and we have been doing is characterizing the major tectonic settings,” says Furlong. “So when an earthquake is imminent, we don’t need a lot of time for the background.”
In essence, they are creating a library of information about earthquake faults and have completed the first level, a general set of information on areas such as Japan, South America, and the Caribbean. Now they are creating the levels of north and south Japan or Chile, Peru, and Ecuador.
Knowing where the old earthquake occurred, how large it was, and how long ago it happened, the researchers could look at the foreshocks, see how much stress they relieved and anticipate, at least in a small way, what would happen.
“This is what we need to do in the future in near real time for decision-makers,” says Furlong.
The National Science Foundation and the USGS supported the research.
Source: Penn State