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A review of the stratigraphic and tectonic development of the Sukhothai Terrane: Implications for the Indosinian-Cimmerian Orogeny
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DOI：10.1016/j.earscirev.2026.105631.png)
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Abstract
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• Sukhothai Permo-Triassic deposits tectono-strat. settings revised to reflect changing plate convergence and collision conditions. • The Sukhothai Terrane developed prior to Carboniferous independently from Indochina. • Just prior to collision (240–250 Ma) plate acceleration caused volcanic flair up in Sukhothai and Indochina arcs. • Complex, long (>150 Ma), Nan Ocean history indicates it is not a simple back-arc basin. • Sukhothai Terrane-Sibumasu collision c. 235 Ma, Norian extensional collapse and soft collision (c. 205 Ma) with Indochina.
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