Spatial-temporal framework for the closure of the Junggar Ocean in central Asia: New SIMS zircon U-Pb ages of the ophiolitic m茅lange and collisional igneous rocks in the Zhifang area, East Junggar
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文摘

The Yemaquan arc and Junggar block collided at approximately 343–348 Ma.

The Junggar Ocean scissors-likely opened from west towards east and closed from east towards west.

The Junggar orogenic belt went through post-collisional extensional stage after 320 Ma.

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