| Citation: | Zhipeng Xie, Chuandong Xue, Tiannan Yang, Wei Wang, Di Xin. Geochemistry and Detrital Zircon U-Pb Geochronology of Lower Carboniferous Clastic Sedimentary Rocks in the Changning-Menglian Belt: Implications for the Evolution of the Paleo-Tethys Ocean. Journal of Earth Science, 2025, 36(3): 910-929. doi: 10.1007/s12583-022-1659-4
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Lower Carboniferous clastic sedimentary rocks (i.e., the Nanduan Formation) in the Changning-Menglian belt of the southeastern Tibetan Plateau may provide new insights into the tectonic evolution of the Paleo-Tethys Ocean. This paper presents new petrographic, geochemical, and detrital zircon U-Pb age data to constrain the provenance and depositional setting of these rocks. Sandstone samples of the Nanduan Formation are all quartz arenites (Q92–99F1–7L0–2) with high SiO2 contents (85.1 wt.%–95.2 wt.%; average = 90.9 wt.%), indicating high compositional maturity. They exhibit fractionated rare earth element (REE) patterns, with light REE enrichment [(La/Yb)N = 6.48-12.1] and negative Eu anomalies (Eu/Eu* = 0.53–0.74), and marked negative Sr-Cs-V-Cr-Ni anomalies in upper continental crust-normalised multi-element diagrams. The geochemical features and heavy mineral assemblages suggest that sediments were mainly derived from ancient sedimentary rocks in cratonic interiors or stable continental areas, and were probably deposited in a passive continental margin setting. Detrital zircon U-Pb dating (
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