Which is heterogeneous, stress or strength? An estimation from high-density seismic observations
Abstract Using data from high-density seismic observation networks installed in the western Nagano Prefecture region in Japan, we precisely determined focal mechanisms and estimated the high-resolution stress field at a scale of 1 km. Almost all differences between observed and calculated slip direc...
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doaj-7d81d3d3ef3c42729f7fd7202d62250b2020-11-24T22:15:54ZengSpringerOpenEarth, Planets and Space1880-59812017-10-0169111610.1186/s40623-017-0730-3Which is heterogeneous, stress or strength? An estimation from high-density seismic observationsYoshihisa Iio0Itaru Yoneda1Masayo Sawada2Tsutomu Miura3Hiroshi Katao4Yoichiro Takada5Kentaro Omura6Shigeki Horiuchi7Research Center for Earthquake Prediction, Disaster Prevention Research Institute, Kyoto UniversityResearch Center for Earthquake Prediction, Disaster Prevention Research Institute, Kyoto UniversityResearch Center for Earthquake Prediction, Disaster Prevention Research Institute, Kyoto UniversityResearch Center for Earthquake Prediction, Disaster Prevention Research Institute, Kyoto UniversityResearch Center for Earthquake Prediction, Disaster Prevention Research Institute, Kyoto UniversityDepartment of Earth and Planetary Sciences, Hokkaido UniversityNational Research Institute for Earth Science and Disaster PreventionHome SeismometerAbstract Using data from high-density seismic observation networks installed in the western Nagano Prefecture region in Japan, we precisely determined focal mechanisms and estimated the high-resolution stress field at a scale of 1 km. Almost all differences between observed and calculated slip directions (misfit) were smaller than the errors in focal mechanisms at grid points away from the mainshock fault. This finding clearly indicates that the estimated uniform stress suitably explains focal mechanisms in each subregion apart from the mainshock fault. Misfits are relatively large at grid points near the mainshock fault, but many of these misfits are smaller than the errors in focal mechanisms, and stress is regarded as uniform for a greater portion within each subregion. However, we found that focal mechanisms and P-axes varied widely and differed from each other for a short focal distance of 100 m. These results clearly show that stress can be regarded as uniform, but that strength is heterogeneous.http://link.springer.com/article/10.1186/s40623-017-0730-3StressHeterogeneityFault strengthStress inversionFocal mechanism |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Yoshihisa Iio Itaru Yoneda Masayo Sawada Tsutomu Miura Hiroshi Katao Yoichiro Takada Kentaro Omura Shigeki Horiuchi |
spellingShingle |
Yoshihisa Iio Itaru Yoneda Masayo Sawada Tsutomu Miura Hiroshi Katao Yoichiro Takada Kentaro Omura Shigeki Horiuchi Which is heterogeneous, stress or strength? An estimation from high-density seismic observations Earth, Planets and Space Stress Heterogeneity Fault strength Stress inversion Focal mechanism |
author_facet |
Yoshihisa Iio Itaru Yoneda Masayo Sawada Tsutomu Miura Hiroshi Katao Yoichiro Takada Kentaro Omura Shigeki Horiuchi |
author_sort |
Yoshihisa Iio |
title |
Which is heterogeneous, stress or strength? An estimation from high-density seismic observations |
title_short |
Which is heterogeneous, stress or strength? An estimation from high-density seismic observations |
title_full |
Which is heterogeneous, stress or strength? An estimation from high-density seismic observations |
title_fullStr |
Which is heterogeneous, stress or strength? An estimation from high-density seismic observations |
title_full_unstemmed |
Which is heterogeneous, stress or strength? An estimation from high-density seismic observations |
title_sort |
which is heterogeneous, stress or strength? an estimation from high-density seismic observations |
publisher |
SpringerOpen |
series |
Earth, Planets and Space |
issn |
1880-5981 |
publishDate |
2017-10-01 |
description |
Abstract Using data from high-density seismic observation networks installed in the western Nagano Prefecture region in Japan, we precisely determined focal mechanisms and estimated the high-resolution stress field at a scale of 1 km. Almost all differences between observed and calculated slip directions (misfit) were smaller than the errors in focal mechanisms at grid points away from the mainshock fault. This finding clearly indicates that the estimated uniform stress suitably explains focal mechanisms in each subregion apart from the mainshock fault. Misfits are relatively large at grid points near the mainshock fault, but many of these misfits are smaller than the errors in focal mechanisms, and stress is regarded as uniform for a greater portion within each subregion. However, we found that focal mechanisms and P-axes varied widely and differed from each other for a short focal distance of 100 m. These results clearly show that stress can be regarded as uniform, but that strength is heterogeneous. |
topic |
Stress Heterogeneity Fault strength Stress inversion Focal mechanism |
url |
http://link.springer.com/article/10.1186/s40623-017-0730-3 |
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