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Paleoproterozoic protracted collisional orogeny: Insights from the Wutai Complex in the central North China Craton
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DOI：10.1016/j.precamres.2026.108130.png)
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Abstract
En 中文
• Metapelites record a clockwise P–T–t–D path during crustal thickening and exhumation. • Metamorphic zircon U–Pb age and biotite Rb–Sr ages were reported. • A protracted orogenic collision and exhumation process is supported.
Keywords:
Paleoproterozoic
collisional orogeny
metamorphic zircon
U–Pb age
exhumation
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3.2
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5.6K
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2.3W
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