Structural overprints of early Paleozoic arc-related intrusive rocks in the Chinese Central Tianshan: Implications for Paleozoic accretionary tectonics in SW Central Asian Orogenic Belts
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文摘

Arc-related magmatism in Central Tianshan occurred in 450–420 Ma and ceased at 417–400 Ma.

Top-to-the-north ductile shearing deformed the early Paleozoic arc-type intrusions.

Mid-late Paleozoic intrusions were free from regional N–S compressive ductile deformation.

Early Carboniferous amalgamation of the Central Tianshan and Tarim is proposed.

Paleozoic intrusive rocks were locally mylonitized due to Permian transcurrent tectonics.

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