Granitic magmatism and tectonic evolution in the Qilian Mountain Range in NW China: A review

doi:10.13745/j.esf.sf.2021.10.39

Abstract

Abstract:

The Qilian Mountain is a composite orogenic belt that has experienced multicyclic tectonic movements, and granitic magmatism plays an important role in the tectonic evolution of such an orogenic belt. According to zircon U-Pb geochronology results, granitic magmatism in the Qilian Mountain can be divided into seven major stages. The Early Paleoproterozoic (2470-2348 Ma) granitic magmatism is related to high-K calc-alkaline strongly peraluminous S-type granites and tholeiitic to high-K calc-alkaline metaluminous I-type granites, which recorded the crustal accretion and transformation events of this period. The Late Paleoproterozoic (1778-1763 Ma) granitic magmatism is predominantly associated with high-K calc-alkaline shoshonitic metaluminous to weakly peraluminous A-type granites formed as a result of the breakup of the Columbia supercontinent. The Late Mesoproterozoic to Early Neoproterozoic (1192-888 Ma) granitic magmatism is mainly related to calc-alkaline shoshonitic peraluminous to strongly peraluminous S-type granites, while the Middle Neoproterozoic (853-736 Ma) granitic magmatism is primarily associated with calc-alkaline to high-K calc-alkaline metaluminous to strongly peraluminous A-type granites, and, respectively, they correspond to the assembly and breakup of the Rodinia supercontinent. The Middle Cambrian to Silurian (516-419 Ma) granitoids are formed during ocean-continent transition, whilst the widely distributed low-Mg adakites (Ca. 440 Ma), derived from the partial melting of thickened crust, indicate the Qilian orogenic belt had fully entered the collisional orogenic period. The Devonian to Early Carboniferous (418-350 Ma) granitoids are formed in the post-collisional environment and consist a series of granites with rock types ranging from tholeiitic to shoshonitic, metaluminous to strongly peraluminous. The Middle Permian to Late Triassic (271-211 Ma) granitoids are dominated by calc-alkaline to high-K calc-alkaline metaluminous to weakly peraluminous I-type granites, with small amounts of high-K calc-alkaline weakly peraluminous A-type granites; respectively, these two types are associated with oceanic subduction and post-collisional extension.

Key words: geochronology, geochemistry, spatial-temporal distribution, granite, Qilian Mountain

CLC Number:

P597

ZHU Xiaohui, CHEN Danling, FENG Yimin, REN Yunfei, ZHANG Xin. Granitic magmatism and tectonic evolution in the Qilian Mountain Range in NW China: A review[J]. Earth Science Frontiers, 2022, 29(2): 241-260.

Figures/Tables 8

Fig.1 Spatial-temporal distribution of granitoids in the Qilian Mountain

Fig.2 Discrimination diagrams for Proterozoic granitoids from the Qilian Mountain. Adapted from [78-81].

Fig.3 Summary of ages and Nd-Hf isotopic compositions for Proterozoic granitoids from the Qilian Mountain

Fig.4 Discrimination diagrams for Early Paleozoic granitoids from the Qilian Mountain. Adapted from [78-81].

Fig.5 Summary of ages and Nd-Hf isotopic compositions for Early Paleozoic granitoids from the Qilian Mountain

Fig.6 Discrimination diagrams for Late Paleozoic-Mesozoic granitoids from the Qilian Mountain. Adapted from [78-81].

Fig.7 Summary of ages and Nd-Hf isotopic compositions for Late Paleozoic-Mesozoic granitoids from the Qilian Mountain

Fig.8 Chronological framework of granitic magmatism in the Qilian Mountain

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