The early–middle Silurian Delite monzogranite and quartz syenite, East Kunlun Orogenic Belt, NW China: petrogenesis and implications for tectonic evolution of the Proto‑Tethys

The tectonic evolution of the Proto‑Tethys in the East Kunlun Orogenic Belt (EKOB) is controversial. Herein, new petrological, whole-rock geochemical, zircon U–Pb geochronological and zircon Lu–Hf isotopic data for early Paleozoic intrusive rocks in the Delite region are reported. LA-ICP-MS zircon U–Pb isotopic data show that the Delite monzogranite and quartz syenite were formed at 437.0 ± 2.9 Ma and 424.8 ± 2.2 Ma, respectively. The Delite monzogranite contains high SiO₂, Al₂O₃ and K₂O and A/CNK ratios, but low MgO and Mg# values (33–38). This study considers that the monzogranite is a typical S-type granite and originated from partial melting of ancient crustal clastic material (metagreywacke) in a syn-collision setting. The quartz syenite is K-rich and Mg-poor, with low Mg# values (36–41), exhibiting geochemical signatures of an alkalic syenite derived from partial melting of basaltic lower crust in a post-collision setting. Combining with the previous work, we suggest that in the middle part of the EKOB the Proto-Tethys closed at <i>ca</i> 437 Ma with a post-collisional setting after <i>ca</i> 427 Ma. KEY POINTSZircons LA-ICP-MS U–Pb isotopic data indicate that the Delite monzogranite and quartz syenite were formed at 437.0 ± 2.9 Ma and 424.8 ± 2.2 Ma, respectively.The Delite monzogranite was formed in a syn-collision setting. The Delite quartz syenite was related to the post-collision setting.It is suggested that the Proto-Tethys closed at <i>ca</i> 437 Ma in the middle part of the EKOB, and the post-collisional setting was after <i>ca</i> 427 Ma in the EKOB. Zircons LA-ICP-MS U–Pb isotopic data indicate that the Delite monzogranite and quartz syenite were formed at 437.0 ± 2.9 Ma and 424.8 ± 2.2 Ma, respectively. The Delite monzogranite was formed in a syn-collision setting. The Delite quartz syenite was related to the post-collision setting. It is suggested that the Proto-Tethys closed at <i>ca</i> 437 Ma in the middle part of the EKOB, and the post-collisional setting was after <i>ca</i> 427 Ma in the EKOB.