PIA06310: Shahdad, Southeast Iran, Radar Interferometry -- Silent Earthquake, Perspective View
 Target Name:  Earth
 Is a satellite of:  Sol (our sun)
 Mission:  European Remote Sensing Satellite Mission (ERS) 
 Spacecraft:  ERS-2
 Instrument:  Synthetic Aperture Radar (SAR) 
Thematic Mapper (TM) 
 Product Size:  1473 x 1200 pixels (w x h)
 Produced By:  JPL
 Full-Res TIFF:  PIA06310.tif (4.672 MB)
 Full-Res JPEG:  PIA06310.jpg (367.1 kB)

Click on the image above to download a moderately sized image in JPEG format (possibly reduced in size from original)

Original Caption Released with Image:

A magnitude 6.6 earthquake struck a sparsely inhabited area of southeast Iran on March 14, 1998, at 11:10 p.m. local time. There were three previous large (magnitudes 5.9 to 7.1) earthquakes since 1981 in this same area around the towns of Sirch, Fandoqa and Gowk. Scientists from NASA's Jet Propulsion Laboratory, Pasadena, Calif., and the Centre for Observation and Modelling of Earthquakes and Tectonics (University of Oxford, UK and the University of Cambridge, UK) and Stanford University used interferometric analysis of radar data from the European Remote Sensing satellites and seismology to study the fault rupture of the 1998 earthquake. The interferometric analysis was performed with software developed at JPL.

The surprising result from the radar interferometry was the discovery that another fault, some 10 to 30 kilometers (6 to 19 miles) to the east of the fault that ruptured in the 1998 earthquake, also moved during the six months after the earthquake. This second fault to the east of the 1998 earthquake has been called the Shahdad thrust fault after the town of Shahdad. The Shahdad thrust fault slip did not cause any detectable seismic waves, but the large area affected and the amount of slip would have been equivalent to a magnitude 6.0 earthquake if it had caused seismic waves. Because there were no seismic waves caused by the slip on the Shahdad thrust fault, it has been called "aseismic" or a "silent earthquake." Calculations of the transfer of stress in the Earth indicate that the March 1998 earthquake probably caused the slip on the Shahdad fault, and that the additional stresses were released by the "silent" slip. If other thrust faults like the Shahdad thrust in places like Los Angeles manage to move silently (or "aseismically"), then they might release stresses that would otherwise build up to cause earthquakes.

The two images show the same three-dimensional perspective view with a Landsat image showing the surface geology in the top image, and the radar interferometry data showing the surface deformation in the bottom image. The town of Shahdad is at the right edge (north) of the images, which are each roughly 50 kilometers (30 miles) wide. In the top image, the light gray linear features running from lower left to upper right across the scene are small ridges that are related to the Shahdad thrust fault. The rainbow colors in the bottom image show contours of the motion of the surface. The big loops in the red tones sweeping out across the low ridges of the Shahdad thrust fault area show the area where the Shahdad fault slipped beneath the surface, with motion towards the east (front of the perspective view). The 1998 earthquake struck a valley on the other side of the mountains in the background of this view.

For more information, see the following paper, published recently in the journal Geology:

Fielding, E.J., Wright, T.J., Muller, J., Parsons, B.E. and Walker, R. (2004), Aseismic deformation of a fold-and-thrust belt imaged by SAR interferometry near Shahdad, southeast Iran, v. 32, no. 7.

The full paper is available (subscription required) at http://www.gsajournals.org/perlserv/?request=get-document&doi=10.1130%2FG20452.1 and for United States Government research a reprint is available at:http://trs-new.jpl.nasa.gov/dspace/handle/2014/6130.

Radar data used in this research were acquired by the European Remote Sensing (ERS) satellites operated by the European Space Agency, which kindly made this data available for research. Part of this research was performed at the Jet Propulsion Laboratory, California Institute of Technology under contract with the U.S. National Aeronautics and Space Administration. Research was also performed at the Centre for the Observation and Modelling of Earthquakes and Tectonics supported by the U.K. Natural Environment Research Council, and at Stanford University. Landsat has been providing visible and infrared views of the Earth since 1972. The Landsat archive is managed by the U.S. Geological Survey's Eros Data Center (USGS EDC).

Size: View is approximately 50 kilometers (30 miles) wide and scale varies in this perspective
Location: 30.0 degrees North latitude, 58.0 degrees East longitude
Orientation: View to the west, 2 times vertical exaggeration. North is to the right
Image Data: Landsat Bands 5, 4, 2 as red, green, blue, respectively (Top). ERS radar interferometric motion contours, 28 millimeters (1 inch) per contour (Bottom)
Image resolution: Landsat: 30 meters (98 feet), Radar: 40 meters (131 feet)
Dates Acquired: May 27, 1996 and September 14, 1998 (ERS radar)

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