1. 1) 東北電力 : 東通原子力発電所敷地内断層の活動性等の評価に係る追加地質調査報告書，添付資料-7 第四系に認められる変状の成因, https://www.tohoku-epco.co.jp/whats/news/2014/0117/index.html. [Tohoku Electric Power Co., Inc.: Additional geological investigation report on the assessments including the activity of faults on the Higashidori Nuclear Power Plant site, accompanying material 7, Factors in the formation of deformation in the stratum formed during the Quaternary]
2. 2) 地震調査研究推進本部：震源断層を特定した地震の強震動予測手法（レシピ）, https://www.jishin.go.jp/evaluation/strong-motion/ strong-motion-recipe. [The Headquarters for Earthquake Research Promotion: Strong ground motion prediction method for earthquakes with specified source faults (Recipe)]
3. 3) 原子力安全推進協会 : 原子力発電所敷地内断層の変位に対する評価手法に関する調査・検討報告書，JANSI-FED-01 rev. 1, 2005. [Japan Nuclear Safety Institute: Report on the investigation and study of evaluation methods for the displacement of faults within the nuclear power plant site, JANSI-FED-01 rev. 1, 2005.]
4. 4) 水本学千，坪井利弘，三浦房紀 : 3次元FEMによる断層モデルの解析に関する基礎的検討，土木学会論文集，No. 780/I-70, pp. 27–40, 2005. [Mizumoto, T., Tsuboi, T. and Miura, F.: Fundamental study on fault rupture process and earthquake motions on and near a fault by 3D-FEM, Journal of JSCE, No. 780 / I-70, pp. 27-40, 2005.]
5. 5) Noe, D. C., Higgins, J. D. and Olsen, H. W. : Steeply dipping heaving bedrock, Colorado: Part 3 - Environmental controls and heaving processes, Environmental and Engineering Geoscience, pp. 325–344, 2007.