Looking Behind the Scenes of a Deadly Earthquake
|
click to enlarge |
| An ALOS Phased Array type L-band Synthetic Aperture Radar (PALSAR) interferogram shows the surface deformation associated with the 2008 Wenchuan earthquake. The white curves depict traces of fault surface breaks. Courtesy of Jianbao Sun; ALOS data: JAXA |
Using satellite radar data and GPS measurements, Chinese researchers have explained the exceptional geological events leading to the 2008 Wenchuan Earthquake that killed nearly 90,000 people in China’s Sichuan Province. Applying a technique called SAR interferometry (InSAR), the researchers produced a set of ‘interferogram’ images covering the entire coseismic rupture region and its vicinity. This interferometric map revealed the amount and scope of surface deformation produced by the earthquake.
“One of the very fundamental issues for understanding an earthquake is to know how the rupture is distributed on the fault plane, which is directly related to the amount of ground shaking and the damage it could cause at the surface,” said Jianbao Sun of the Institute of Geology, China Earthquake Administration (IGCEA).
To learn this, Sun and Zhengkang Shen of IGCEA and Peking University’s Department of Geophysics, and collaborators acquired two kinds of satellite radar data: advanced synthetic aperture radar (ASAR) data in C-band from ESA’s Envisat satellite and phased array type L-band synthetic aperture radar (PALSAR) data from Japan’s ALOS satellite.
InSAR involves combining two or more radar images of the same ground location in such a way that very precise measurements — down to a scale of a few centimeters — can be made of any ground motion taking place between image acquisitions. Colored interferograms usually appear as rainbow fringe patterns.
 |
| The clock on the Hangwan Bell Tower stopped forever at 14:28 (06:28 UTC), when the earthquake struck. Courtesy of Fang Liang |
The researchers combined the SAR satellite data with GPS measurements and developed a model that shows fault geometry and rupture distribution of the Longmen Shan fault zone, a series of parallel faults that run for about 400 km from southwest to northeast in the region. The earthquake that struck on May 12, 2008, produced a 240-km-long rupture along the Beichuan fault and a 72-km-long rupture along part of the Pengguan fault.
“This is perhaps the very first time people have seen the complete deformation field produced by an earthquake on such a large scale,” Sun said.
Studying the model, they were able to determine that the fault plane dips considerably to the northwest in the zone’s southwest area and then rises up to a nearly vertical position in the zone’s northeast.
They also learned that the direction of the motion along the fault changed, going from a thrust, where upper layer rocks were pushed up and lower layer rocks pulled down, to a ‘dextral faulting,’ where two parts of Earth’s plates slide past each other. About a seven-meter slip, the greatest along the rupture, was detected on the Beichuan fault near Beichuan City, which was destroyed completely by the quake and suffered the highest number of casualties.
Another major finding was that the fault junctions (solid rock barriers that stop a quake from propagating from one segment to another), beneath the hardest-hit cities of Yingxiu, Beichuan and Nanba, failed to withstand the extraordinary energy released along the fault.
“These fault junctions are barriers, whose failures in a single event allowed the rupture to cascade through several fault segments, resulting in a major 7.9-earthquake,” Shen explained. “Earthquakes across fault segments like this are estimated to happen about every 4,000 years.”
Following the quake, Sun and Shen worked closely with the ‘Dragon 2’ program to coordinate SAR coverage of the seismic area. Dragon 2 is a joint undertaking between ESA and China’s Ministry of Science and Technology that encourages scientists to use satellite data to monitor and understand environmental phenomena in China.
 |
| GPS and InSAR data post fit residuals. The main map and inset map are derived from Phased Array type L-band Synthetic Aperture Radar (PALSAR) data from Japan’s ALOS satellite (main map), Advanced Synthetic Aperture Radar (ASAR) data in C-band from ESA’s Envisat satellite and GPS data. Red arrows and black columns are for the horizontal and vertical components of the GPS displacements. Courtesy of Jianbao Sun, IGCEA; ALOS data: JAXA; Envisat data: ESA |
“The resulting Envisat SAR data acquired along an important track close to the epicenter turned out to be vital in constraining the southern part of the deformation field and helping explain the fault geometry and rupture distribution of the Pengguan fault, which would be difficult to resolve otherwise,” Shen said.
The scientists also hope the data will help to assess earthquake potential in the future.
“Under the coordination of Dragon 2, the SAR data acquired during this period will be used, along with GPS measurements, to reveal geophysical processes within the Longmen Shan fault zone and the lower crust and upper mantle, which will help us understand the earthquake and faulting mechanisms and hopefully shed light on future seismic risks in this area.”
The results were published in the journal Nature Geoscience, part of Nature magazine.
