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Correction: Two pulse intrusive events of the Pliocene Tanigawa-dake granites revealed from zircon U–Pb dating

The Original Article was published on 16 December 2021

Correction to: Earth, Planets and Space (2021) 73:231

Following publication of the original article (Minami et al. 2021), the authors reported some errors in Fig. 1 and Table 1. The authors apologize for these errors and any confusion they may have caused.

The correct Fig. 1 and Table 1 have been provided in this Correction.

Fig. 1
figure 1

Index map of the study area. The geologic map was modified from Sato (2016) and Geological Survey of Japan web page (,36.83525,138.87626). Circle points denote sampling localities. Colored circles denote sampling localities in this study. Sampling sites of the previous studies are shown by the following symbols. Filled square: K–Ar ages of biotite (Kawano et al. 1992; Sato 2016; Shibata et al. 1984), open squares: K–Ar ages of whole rock (Kubo et al. 2013), filled inverted triangles: fission-track ages of zircon (Ohira et al. 1998; Ohira and Honda 1999). Note that the sites of TNG20-10 indicated by a red circle overlap the localities of zircon fission-track and biotite K–Ar ages of the previous researches (Kawano et al. 1992; Ohira et al. 1998; Ohira and Honda 1999; Sato 2016). Similarly, the site of TNG20-09 shown by a navy circle overlap the locality of K–Ar age of the whole rock (Kubo et al. 2013)

Table 1 Summary of dating results

The original article (Minami et al. 2021) has been updated.


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Correspondence to Saki Minami.

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Minami, S., Nagata, M., Sueoka, S. et al. Correction: Two pulse intrusive events of the Pliocene Tanigawa-dake granites revealed from zircon U–Pb dating. Earth Planets Space 74, 129 (2022).

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