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Petrogenesis and tectonomagmatic evolution of diabase dikes in a Tethyan SSZ setting: constraints from U-Pb geochronology, geochemistry and Sr-Nd-Pb isotopes
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DOI：10.1016/j.lithos.2026.108679.png)
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Abstract
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• Titanite U-Pb ages indicate dike crystallization at 89.40 ± 13.40 and 80.47 ± 4.77 Ma. • Sr-Nd-Pb isotopes display subduction-related mantle metasomatism. • Tekirova dikes formed by 1–10% and Gödene dikes by ∼20% melting. • Dikes formed in a SSZ fore-arc during Neotethyan slab roll-back.
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