S.H. White

Pulsed rise and growth of the Tibetan Plateau to its northern margin since ca. 30 Ma

Oxygen isotopes trace the origins of Earth’s earliest continental crust

Palaeomagnetism of flood basalts in the Pilbara Craton, Western Australia: Late Archaean continental drift and the oldest known reversal of the geomagnetic field

Reply to comment on “Evidence for multiphase deformation in the Archaean basal Warrawoona group in the Marble Bar area, East Pilbara, Western Australia” (van Haaften, W.M., White, S.H., 1998. Precambrian Research 88, 53–66) by M.J., Van Kranendonk, A.H. Hickman, W.J., Collins