@article{oai:nagoya.repo.nii.ac.jp:00001415,
 author = {MORISHITA, Taisei and SUZUKI, Kazuhiro},
 journal = {The Journal of earth and planetary sciences, Nagoya University},
 month = {Dec},
 note = {The Shinshiro Tonalite located on the north of the Median Tectonic Line in the Mikawa area is the oldest pluton among the post-tectonic intrusives in the eastern Ryoke belt. Monazites recovered from three samples of the leucocratic varieties of the Shinshiro Tonalite yield CHIME ages of 86.0±4.7,85.2±3.3 and 85.5±5.5 Ma. These ages, interpreted as the time of the emplacement, are some 15 Ma younger than the CHIME monazite ages for the Ryoke gneiss, and slightly older than the CHIME monazite ages for the subsequent Mitsuhashi Granodiorite (ca. 84 Ma)., 国立情報学研究所で電子化したコンテンツを使用している。},
 pages = {45--53},
 title = {CHIME ages of monazite from the Shinshiro Tonalite of the Ryoke belt in the Mikawa area, Aichi Prefecture},
 volume = {42},
 year = {1995}
}