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
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| Description | article by Rupert Sutherland et al published 20 March 2010 in Tectonics |
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author: Vaughan Stagpoole Nick Mortimer Rupert Sutherland Julien Collot Ron Hackney Karen Higgins |
| Publication date | March 20, 2010 |
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