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Lithosphere delamination with foundering of lower crust and mantle caused permanent subsidence of New Caledonia Trough and transient uplift of Lord Howe Rise during Eocene and Oligocene initiation of Tonga-Kermadec subduction, western Pacific
article by Rupert Sutherland et al published 20 March 2010 in Tectonics
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March 20, 2010
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