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Erratum to: Importance of rheological heterogeneity for interpreting viscoelastic relaxation caused by the 2011 Tohoku-Oki earthquake
© The Author(s) 2017
- Received: 28 March 2017
- Accepted: 6 April 2017
- Published: 20 April 2017
The original article was published in Earth, Planets and Space 2017 69:21
Unfortunately, an important reference was missing in the original paper (Suito 2017). Therefore, it is necessary to add a reference. In addition, a sentence in the paper needs to be replaced as follows. It should be noted that all conclusions are not subject to correction.
Page 10, right column, Line 40
“The depth-dependent viscosity structure in this study contained the lowest viscosity at a depth of 150–300 km, which is consistent with these rock rheological estimates.” should be replaced as: “The depth-dependent viscosity structure in this study contained the lowest viscosity at a depth of 150–300 km, which is consistent with these rock rheological estimates. Recently published paper of Freed et al. (2017) regarding the postseismic deformation following the 2011 Tohoku-Oki earthquake also reported similar depth-dependent structure.”
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- Freed AM, Hashima A, Becker TW, Okaya DA, Sato H, Hatanaka Y (2017) Resolving depth-dependent subduction zone viscosity and afterslip from postseismic displacements following the 2011 Tohoku-oki, Japan earthquake. Earth Planet Sci Lett 459:279–290. doi:10.1016/j.epsl.2016.11.040 View ArticleGoogle Scholar
- Suito H (2017) Importance of rheological heterogeneity for interpreting viscoelastic relaxation caused by the 2011 Tohoku-Oki earthquake. Earth Planet Space 69:21. doi:10.1186/s40623-017-0611-9 View ArticleGoogle Scholar