| Citation: | Shi-Heng Bai, Ru-Xiong Lei, Matthew J. Brzozowski, Zhen-Hua Wang, Wei Wang, Chang-Zhi Wu. Permian Ridge Subduction-Related Magmatism in the Chinese Altai: Insights from Geochronology and Geochemistry of the Jiangjunshan Pluton. Journal of Earth Science, 2025, 36(6): 2479-2497. doi: 10.1007/s12583-024-0088-y |
The Chinese Altai, a key component of the Central Asian Orogenic Belt (CAOB), represents a significant Phanerozoic accretionary orogenic belt. The oceanic-continental subduction processes spanning the Cambrian to Carboniferous and subsequent intracontinental extension since the Triassic have been well documented in the Chinese Altai, the southwestern segment of the CAOB. Deciphering the petrogenetic evolution of this region during the Permian is thus crucial for advancing our understanding of its tectonic transitions. However, the Permian tectonic setting of the Chinese Altai remains contentious. To address this knowledge gap, this study presents new geochronological and geochemical data for the Jiangjunshan pluton in the southern Chinese Altai. Zircon U-Pb geochronology reveals that the gabbro and two-mica alkali feldspar granite—which collectively constitute the primary lithology of the Jiangjunshan pluton—were emplaced at ~272 ± 3.5 and ~272 ± 1.6 Ma, respectively. Geochemically, the gabbro exhibits pronounced light rare-earth element (LREE) depletion, low Nb/Yb (0.39–0.46) and Ti/V (23.7–25.3) ratios, and trace-element signatures akin to normal mid-ocean ridge basalts (N-MORB). However, its conspicuous Nb-Ta depletion parallels that of island arc basalts. Depleted Hf-Nd isotopic compositions (
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