Changes in the b value in and around the focal areas of the M6.9 and M6.8 earthquakes off the coast of Miyagi prefecture, Japan, in 2021

• Published in: Earth, planets, and space Vol. 73; no. 1; pp. 1 - 10
• Main Authors: Nanjo, K. Z., Yoshida, A.
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 14.09.2021; Springer; Springer Nature B.V; SpringerOpen
• Subjects: 4. Seismology; and prediction; Earth and Environmental Science; Earth Sciences; Earthquake dynamics; Earthquake intensity; Earthquake interaction; Earthquakes; Express Letter; forecasting; Geology; Geophysics/Geodesy; Japan; Measurement; Observations; Projects; Seismic activity; Seismicity; Seismicity and tectonics; Seismological research; Slip; Statistical analysis; Stress; Japan; and prediction; Stresses; Subduction zone processes; Statistical analysis; Time series analysis; forecasting; Earthquake dynamics; Computational seismology; Spatial analysis; Earthquake interaction; Seismicity and tectonics
• ISSN: 1880-5981; 1343-8832; 1880-5981
• DOI: 10.1186/s40623-021-01511-3

We investigated changes in the b value of the Gutenberg–Richter’s law in and around the focal areas of earthquakes on March 20 and on May 1, 2021, with magnitude ( M ) 6.9 and 6.8, respectively, which occurred off the Pacific coast of Miyagi prefecture, northeastern Japan. We showed that the b value in these focal areas had been noticeably small, especially within a few years before the occurrence of the M 6.9 earthquake in its vicinity, indicating that differential stress had been high in the focal areas. The coseismic slip of the 2011 Tohoku earthquake seems to have stopped just short of the east side of the focus of the M 6.9 earthquake. Furthermore, the afterslip of the 2011 Tohoku earthquake was relatively small in the focal areas of the M 6.9 and M 6.8 earthquakes, compared to the surrounding regions. In addition, the focus of the M 6.9 earthquake was situated close to the border point where the interplate slip in the period from 2012 through 2021 has been considerably larger on the northern side than on the southern side. The high-stress state inferred by the b -value analysis is concordant with those characteristics of interplate slip events. We found that the M 6.8 earthquake on May 1 occurred near an area where the b value remained small, even after the M 6.9 quake. The ruptured areas by the two earthquakes now seem to almost coincide with the small- b -value region that had existed before their occurrence. The b value on the east side of the focal areas of the M 6.9 and M 6.8 earthquakes which corresponds to the eastern part of the source region of the 1978 off-Miyagi prefecture earthquake was consistently large, while the seismicity enhanced by the two earthquakes also shows a large b value, implying that stress in the region has not been very high.