Petrogenesis of the early Paleozoic low-Mg and high-Mg adakitic rocks in the North Qilian orogenic belt, NW China: Implications for transition from crustal thickening to extension thinning

Abstract The petrogenesis and geodynamic implications of the early Paleozoic adakitic rocks in the North Qilian orogenic belt remain topics of debate. In this study, petrology, zircon U–Pb age and Lu–Hf isotopic composition, whole-rock geochemistry and Sr–Nd isotopes were carried on both low-Mg and high-Mg adakitic rocks from the North Qilian orogenic belt. These results will provide significant constraints on the evolution of the North Qilian orogenic belt. In general, the low-Mg adakitic granites mainly consist of plagioclase (50–55%), alkali feldspar (20–25%), quartz (20–25%) and biotite (5%). In contrast, the high-Mg adakitic granodiorites are generally composed of alkali feldspar (30–35%), plagioclase (30–45%), quartz (20–25%) and amphibole (∼10%). The low-Mg adakitic granitoids (446–457 Ma) are characterized by high SiO 2 (69–72 wt.%), low Mg # (39–42) and low Cr and Ni contents. However, the high-Mg adakitic granitoids (430–431 Ma) have relatively lower SiO 2 (65–66 wt.%), higher Mg # (50–59) and higher Cr and Ni contents. The low-Mg adakitic rocks have high initial 87 Sr/ 86 Sr ratios (0.7068–0.7080), negative e Nd ( t ) (−2.3 to −3.3) and e Hf ( t ) values (−6.8 to 1.9) with old zircon Hf model ages (1.2–1.6 Ga). However, the high-Mg adakitic rocks show lower initial 87 Sr/ 86 Sr ratios (0.7044–0.7066), higher e Nd ( t ) (−1.8 to 3.0) and positive e Hf ( t ) values (2.3–7.7) with younger zircon Hf model ages (0.9–1.1 Ga). These results suggest that the low-Mg rocks were generated by partial melting of thickened crust, whereas the high-Mg rocks were derived from anatexis of delaminated lower crust, which subsequently interacted with mantle magma upon ascent. The data obtained in this study provide significant information about the geological and tectonic processes after the closure of the Qilian Ocean. The continent–continent collision and thickening probably occurred during 440–467 Ma with formation of low-Mg adakitic rocks; and the transition of the tectonic regime from compression to extension probably occurred at ∼430 Ma with formation of high-Mg adakitic rocks.