The storage of water at the mantle boundary layer (MBL) of 410-660 km with time leads to continental breakup during or after formation of supercontinent, say, 250 m.y. after the present. Sequential change of magmatic activity from kimberlite and/or carbonatite, through flood basalt to MORB,...
Mineral evolution: episodic metallogenesis, the supercontinent cycle, and the coevolving geosphere and biosphere Soc. Econ. Geol. Spec. Publ., 18 (2014), pp. 1-15 Google Scholar Hazen et al., 2015a R.M. Hazen, E.S. Grew, R.T. Downs, J. Golden, G. Hystad Mineral ecology: chance ...
Rosas (2018), The future of earth's oceans: Consequences of subduction initiation in the atlantic and implications for supercontinent formation, Geological Magazine, 155, 45-58.Duarte, J., Schellart, W., & Rosas, F. (2018). The future of Earth's oceans: Consequences of subduction ...