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Extra resources for Paleozoic and Mesozoic tectonic evolution of central Asia: from continental assembly to intracontinental deformation, Nummer 194
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And is not yet complete. Applying these observations to the late Paleozoic Tian Shan, we envision an initial encounter between Tarim and the central Tian Shan occurring near the Devonian-Carboniferous boundary (perhaps reflected in the Devonian-Carboniferous unconformity observed in northern Tarim and the central Tian Shan), with subsequent rotational closure of the south Tian Shan remnant ocean basin throughout the Early Carboniferous accounting for blueschist-metamorphic and arc-igneous radiometric ages in the paired belts of the southern central Tian Shan (Fig.