Conceptual cross-section illustrating fromation of the Bentong-raub Suture by subduction of the Palaeo-Tethys Ocean and collision of the Sibumasu and Indochina terranes. Palaeo-Tethys opened in the Devonian, when Indochina and other Chinese blocks separated from Gondwana (in the late Sakmarian, Permian) and closed in the Late Triassic (After Metcalfe, 2000).
May 13, 2009
May 3, 2009
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