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Migrating intracontinental orogeny recorded by diachronous regional unconformities
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DOI：10.1016/j.epsl.2026.120254.png)
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Abstract
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• Diachronous deformation and magmatism identified in North China Craton. • Subduction geometry drives intracontinental orogeny far from plate boundaries. • Unconformities redefined as dynamic features linking subduction to surface deformation.
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