Correction to: Switching from seismic faulting to silent slips in harzburgite induced by H 2 O fluid at upper mantle pre
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CORRECTION
Correction to: Switching from seismic faulting to silent slips in harzburgite induced by H2O fluid at upper mantle pressures T. Ohuchi1 · X. Lei2 · Y. Higo3 · Y. Tange3 · T. Sakai1 Published online: 16 August 2020 © Springer-Verlag GmbH Germany, part of Springer Nature 2020
Correction to: Contributions to Mineralogy and Petrology https://doi.org/10.1007/s00410-020-01716-x
In the original version of the article, the Fig. 2 was published incorrectly. The corrected Fig. 2 is provided in this correction.
The original article can be found online at https://doi.org/10.1007/ s00410-020-01716-x. * T. Ohuchi [email protected]‑u.ac.jp 1
Geodynamics Research Center, Ehime University, Matsuyama 790‑8577, Japan
2
Geological Survey of Japan, National Institute for Advanced Industrial Science and Technology, Tsukuba 305‑8567, Japan
3
Japan Synchrotron Radiation Research Institute, Sayo, Hyogo 679‑5198, Japan
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Fig. 2 Representative stress, pressure, strain, and continuous acoustic records in harzburgite samples deformed at 960 K. a A fluid-bearing sample (M2182). b A fluid-free sample (M2065). The stress values were obtained from five diffraction peaks of olivine (solid circle: 020, solid diamond: 021, solid square: 101, solid triangle: 130; open triangle: 131). Pressure is shown by gray open circles. The cumulative number of AEs (gray line) and AE amplitudes (red impulses: AEs from the inside of the sample; green impulses: outside of the sample) are plotted as a function of time. AE data from the outside of the sample are also shown here to demonstrate that AE monitoring was continued during the deformation runs. The total number of AE
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events (Ni: from the inside of the sample: No: outside of the sample) is also shown. The timing when a fault occurred is shown by a thick blue-dashed line. The highest strain rate probably due to fault slip is shown by a pink arrow. c, d Representative three-dimensional views of AE hypocenters in deforming harzburgites (c M2182; d M2065). Positions of the (Mg, Co)O pressure medium are shown by a cube (black lines). The sample region before the deformation is shown by a blue cylinder. Red and green dots are the positions of AE hypocenters (red: sample inside; green: outside of the sample). Arrows represent the compressional direction. Black lines represent the range of location error
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