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Tectonic transition from Late Carboniferous subduction to Early Permian post-collisional extension in the Eastern Tianshan, NW China: Insights from geochronology and geochemistry of mafic-intermediate intrusions
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文摘

310–290 Ma mafic–intermediate rocks were discovered in the Central Tianshan block.

Late Carboniferous intrusions were emplaced in a continental arc setting.

Early Permian within-plate magmatism was linked to post-collisional slab break-off.

The Junggar Ocean most probably closed in the latest Carboniferous.

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