1. Barker, P.F., 1982, The Cenozoic subduction history of the Pacific margin of the Antarctic Peninsula: ridge crest-trench interactions. Journal of Geological Society of London, 139, 787–801.
2. Blichert-Toft, J., Albarède, F. and Kornprobst, J., 1999, Lu-Hf isotope systematics of garnet pyroxenites from Beni Bousra, Morocco: Implications for basalt origin. Science, 283, 1303–1306.
3. Choe, W.H., Lee, J.I., Lee, M.J., Hur, S.D. and Jin, Y.K., 2005, New approach on the extinction of spreading at the Phoenix Ridge, Antarctica. Journal of the Petrological Society of Korea, 14, 73–81. (in Korean with English Abstract).
4. Cooper, K.M., Eiler, J.M., Asimow, P.D. and Langmuir, C.H., 2004, Oxygen isotope evidence for the origin of enriched mantle beneath the mid-Atlantic ridge. Earth and Planetary Science Letters, 220, 297–316.
5. Donnelly, K.E., Langmuir, C.H. and Goldstein, S.L., 2000, Constraints on the generation of enriched mid-ocean ridge basalts. EOS, 81, 1281.