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

Correction to: Earth, Planets and Space (2021) 73:231 https://doi.org/10.1186/s40623-021-01556-4

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

Index map of the study area. The geologic map was modified from Sato (2016) and Geological Survey of Japan web page (https://gbank.gsj.jp/geonavi/geonavi.php#11,36.83525,138.87626). 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.