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Correction to: Which is heterogeneous, stress or strength? An estimation from high-density seismic observations

The Original Article was published on 20 October 2017

Correction to: Earth, Planets and Space (2017) 69:144 https://doi.org/10.1186/s40623-017-0730-3

After publication of this work (Iio et al. 2017), an error was noticed. FiguresĀ 10 and 12 were accidentally swapped. This was caused due to a typesetting error.

This is now corrected below (Figs.Ā 10, 12):

Fig.Ā 10
figure 10

a Plots of the normalized shear and normal stresses on faults on a three-dimensional Mohr diagram for a grid point (xĀ =Ā 10, yĀ =Ā 9, zĀ =Ā āˆ’Ā 2). Pore pressure indicators Pp are calculated as PpĀ =Ā ĻƒnĀ āˆ’Ā Ļ„/Ī¼, where Ī¼ is assumed as 0.6. Sizes of circles represent the difference of misfits between the fault plane and auxiliary plane (misfitdiff); coloring indicates only data with misfits on the fault plane greater than the error of focal mechanisms, 10Ā°. b Histogram of misfits. c Relationship between azimuths and dip angles of the fault planes. Misfits are also indicated by the sizes and colors of circles. d Relationship between magnitude and misfit. e Histogram of the pore pressure indicator, Pp

Fig.Ā 12
figure 12

a Plots of the normalized shear and normal stresses on a three-dimensional Mohr diagram for a grid point (xĀ =Ā 9, yĀ =Ā 6, zĀ =Ā āˆ’Ā 2). b Histogram of misfits. c Relationship between azimuths and dip angles of the fault planes. d Relationship between magnitude and misfit. e Histogram of the pore pressure indicator Pp. Other explanations are the same as for Fig.Ā 10

The publisher apologises for these errors.

Reference

  • Iio Y, Yoneda I, Sawada M, Miura T, Katao H, Takada Y et al (2017) Which is heterogeneous, stress or strength? An estimation from high-density seismic observations. Earth Planets Space 69:144

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Correspondence to Yoshihisa Iio.

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The original article can be found online at https://doi.org/10.1186/s40623-017-0730-3.

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Iio, Y., Yoneda, I., Sawada, M. et al. Correction to: Which is heterogeneous, stress or strength? An estimation from high-density seismic observations. Earth Planets Space 70, 20 (2018). https://doi.org/10.1186/s40623-018-0778-8

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  • DOI: https://doi.org/10.1186/s40623-018-0778-8