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The Cablac Mountain Range in central East Timor comprises a thrust stack of Gondwana Megasequence rocks, of mainly Triassic to Jurassic age. This southerly-directed thrust stack occurs in structural contact with the underlying Lolotoi Formation, and both the Lolotoi Formation and the overlying Gondwanan thrust stack appear to be structurally emplaced upon younger, mid-Eocene units to the south. In...
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