Cite
Origin of Late Oligocene to Middle Miocene Adakitic Andesites, High Magnesian Andesites and Basalts from the Back-arc Margin of the SW and NE Japan Arcs.
MLA
Sato, M., et al. “Origin of Late Oligocene to Middle Miocene Adakitic Andesites, High Magnesian Andesites and Basalts from the Back-Arc Margin of the SW and NE Japan Arcs.” Journal of Petrology, vol. 54, no. 3, Mar. 2013, pp. 481–524. EBSCOhost, https://doi.org/10.1093/petrology/egs075.
APA
Sato, M., Shuto, K., Uematsu, M., Takahashi, T., Ayabe, M., Takanashi, K., Ishimoto, H., & Kawabata, H. (2013). Origin of Late Oligocene to Middle Miocene Adakitic Andesites, High Magnesian Andesites and Basalts from the Back-arc Margin of the SW and NE Japan Arcs. Journal of Petrology, 54(3), 481–524. https://doi.org/10.1093/petrology/egs075
Chicago
Sato, M., K. Shuto, M. Uematsu, T. Takahashi, M. Ayabe, K. Takanashi, H. Ishimoto, and H. Kawabata. 2013. “Origin of Late Oligocene to Middle Miocene Adakitic Andesites, High Magnesian Andesites and Basalts from the Back-Arc Margin of the SW and NE Japan Arcs.” Journal of Petrology 54 (3): 481–524. doi:10.1093/petrology/egs075.