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Linking zircon (re-)crystallization to partial melting in migmatitic orthogneiss: Constraints on the tectonometamorphic evolution of the Upper Greater Himalayan Sequence, Western Arunachal Himalaya, NE India
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DOI：10.1016/j.lithos.2026.108682.png)
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Abstract
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• The Zimithang thrust (ZT) represents a distinct metamorphic discontinuity. • Zircon petrochronology reveals ZT initiation at <20 Ma. • Hanging wall of the ZT produced 22–29 vol% melt, likely contributing to leucogranites. • Melt-enhanced weakening triggered exhumation of the Upper Greater Himalayan Sequence. • Upper Greater Himalayan Sequence exhumed rapidly during the Early Miocene (~5 mm/yr).
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