1. 足立 守・吉田鎮男, 1984, 丹波帯, 久坂層と古屋層の層序の再検討．DESK総研報告「近畿地方を中心とする後期古生代～古第三紀の堆積盆の変遷」, 4, 16-20. ［Adachi, M. and Yoshida, S., 1984, Re-examination of stratigraphy of the Hisasaka and Furuya Formations in the Tamba Belt. Report of Cooperative Research on DESK（Development of Sedimentary Basins through Late Paleozoic to Paleogene in Kinki and Neighboring District）, 4, 16-20.］ English translation from the original written in Japanese.
2. 縣 孝之, 1974, 大浦複合岩体：舞鶴市・大浦半島の層状貫入岩体についての岩石学的研究．岩鉱, 69, 403-416. ［Agata, T., 1974, Petrological study on the Oura Complex, northern Maizuru City, central Japan. J. Mineral. Petrol. Econ. Geol., 69, 403-416.］
3. Agata, T., 1980, Hornblende-rich gabbro-diorite sequence in the Oura igneous complex, Maizuru City, Japan, Part 1: A generation of late differentiates midway in the layered sequence. J. Mineral. Petrol. Econ. Geol., 75, 396-410.
4. Agata, T., 1981, Hornblende-rich gabbro-diorite sequence in the Oura igneous complex, Maizuru City, Japan, Part 2: Hydrothermal events and genesis of igneous albite. J. Mineral. Petrol. Econ. Geol., 76, 35-48.
5. Blow, W. H., 1969, Late Middle Eocene to recent planktonic foraminiferal biostratigraphy. In Bronnimann, P. and Renz, H. H., eds., Proceedings of First International Conference of Planktonic Microfossils, Geneva, 1967, 1, 199-422.