Petrogenesis of Paleocene–Eocene gabbros in the Gangdese belt: geochemical tracking of transitioning from oceanic subduction to continental collision related magmatism in southern Tibet

The composition of the sub-arc mantle and the mode and nature of geodynamic processes during the India-Asia collision that controlled the melt evolution beneath the Gangdese belt (southern Tibet) are still unclear. Here, we present new U-Pb ages and Hf isotopes of zircon, and whole-rock geochemical and Sr-Nd-Pb isotopic data of the Paleocene–Eocene Najinla gabbros from the East Gangdese magmatic belt, aiming to track the transitioning magmatism formed from oceanic subduction to continental collision in the region. Zircon U-Pb analyses of these mafic rocks yield emplacement ages of 54 ± 1 Ma and 63 ± 1 Ma. The gabbros are characterized by variable SiO₂ (45.87–55.44 wt%), MgO (1.03–8.18 wt%), FeO_T (3.74–12.33 wt%), and Al₂O₃ (13.45– 25.45 wt%) contents. Most samples exhibit high Al₂O₃ (17.15–25.45 wt%) and relatively low MgO (1.03–6.11 wt%), similar to typical high-alumina basalts and high-alumina basaltic andesites. The Najinla gabbros show characteristic subduction-related signatures with enriched large-ion lithophile elements and depleted high field strength elements. They have depleted Sr-Nd isotopic compositions with low and relatively homogeneous initial ⁸⁷Sr/⁸⁶Sr isotopic ratios of 0.7045– 0.7049 and positive ɛ_Nd(t) ratios of +2.2 to +3.2. The Najinla gabbroic rocks also have positive zircon ɛHf(t) values, ranging from +5.6 to +10.9. These results collectively suggest that magmas of the gabbros formed by partial melting of the asthenosphere with negligible crustal contamination during their emplacement. We propose that the mantle source of the Najinla gabbros was strongly influenced and metasomatized by subducted Neotethyan oceanic crust-derived fluids in the mantle wedge. Rollback of the subducted Neotethyan slab in the early Eocene led to partial melting of the subduction-modified mantle and the formation of these gabbros.