1. Asada, M., 2017, Why and where do submarine mud volcano existing? A case study of the Kumano basin, Nankai Trough subduction zone, Japan. JpGU-AGU Joint Meet. 2017, Abstr., SGL34-P04.
2. 浅田美穂・木村俊則・野口拓郎・Moore, G. F., 2015, 熊野外縁隆起帯に発現した泥火山と巨大露頭の音響観測結果速報.InterRidge-Japan研究集会要旨集, O-25. [Asada, M., Kimura, T., Noguchi, T. and Moore, G. F., 2015, Preliminary report of mud volcano and large outcrop at Kumano Basin Edge Fault Zone. InterRidge-Japan Meet. Abstr., O-25.]*
3. 浅田美穂・木村俊則・野口拓郎・Moore, G. F., 2016, 「うらしま」は見た!?熊野海盆外縁隆起帯における泥火山活動の確認とチムニー群の発見.ブルーアース2016要旨集, BE16-P03. [Asada, M., Kimura, T., Noguchi, T., and Moore, G. F., 2016, Verification of mud volcano activity and discovering chimney-like features at the Kumano Basin Edge Fault Zone, based on the acoustic observations using R/V Yokosuka and AUV-Urashima. Blue-Earth Symp. 2016, Abstr., BE16-P03.]*
4. Ashi, J. and Taira, A., 1992, Structure of the Nankai accretionary prism as revealed from IZANAGI sidescan imagery and multichannel seismic reflection profiling. Isl. Arc, 1, 104–115.
5. 芦寿一郎・徳山英一・平 朝彦, 1990, 南海トラフ付加体の微細・中規模地形:海底イメージングソナーIZANAGIを用いた研究.堆積学研究会報, 33, 43–48. [Ashi, J., Tokuyama, H., and Taira, A., 1990, Structure of the Nankai Trough accretionary prism revealed by IZANAGI oceanfloor imaging sonar system. J. Sediment. Soc. Japan, 33, 43–48.]