Fault and geodynamics Research Group
specializing in Rock fracture mechanics, Earth continuum mechanics, and Earthquake prediction
•Professor Norihiro Nakamura,
specializing in Earth and planetary magnetism studies, Magnetic field, and Meteorites
•Associate Professor Jun Muto, specializing in Structural geology, and Experimental rock mechanics
Earthquakes and crustal deformation are complex deformation processes on Earth that occur in non-equilibrium systems where energy is not conserved. By integrating mathematical and physical theories, laboratory rock experiments, and field geological surveys, we aim to achieve a more comprehensive understanding of Earth's deformation processes beyond observational methods and scales.
Looking for faults
Electron microscope analysis of the Nojima Fault, which caused the 1995 Hyogo-ken Nanbu Earthquake, revealed that the fault plane became molten from frictional heating during the earthquake (Fig. 1). Although there are many active faults in Japan, not many of the faults that have caused earthquakes are exposed, so it is necessary to travel to other global sites to examine exposed faults. Figure 2 shows an outcrop of the Alpine Fault in the South Island of New Zealand. This outcrop presents a rare opportunity to see where the Pacific Plate (green rocks on the left) and the Australian Plate (brown rocks on the right) meet on land. The tremendous force of plate collision severely deforms the rocks on both sides.
Figure 1: Flow areas (top) and magnetic anomalies (bottom) developing in the Nojima fault. The red area, billow-like wavy folds, is a magnetic anomaly suggestive of frictional melting of the fault (modified from Fukuzawa et al., 2017).
Figure 2: Outcrop photograph of the NZ Alpine Fault. The Pacific Plate and the Australian Plate are in contact. With Associate Professor Tomoki Okada (Tohoku University, left) and Dr. Rick Sibson (Emeritus Professor, University of Otago, right).
Reproducing fault motion
On the other hand, it is known that when an earthquake occurs, rocks deform at a tremendous strain rate exceeding 1000/s. At such a high strain rate, rocks can be shattered into pieces in an instant (movie). By comparing the shape and particle size distribution of such pulverized samples with natural fault rocks, we investigate the strain rate and energy dissipation process during earthquakes.
Figure 3: Photograph of a miniature fault created in the experiment.
Movie: Rock crushing at high speed experiment
Predicting Earthquakes
Figure 4: Image showing the exhalation of radon gas from underground. The concentration of radon in the atmosphere is measured at radio isotope facilities, where the radon containing gas dissipates to the ground through cracks (fissures) in the bedrock that occur before and after earthquakes.