Geochemical and Re–Os isotope constraints on the origin and age of the Songshugou peridotite massif in the Qinling orogen, central China
发布时间：2024-05-31
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- Lithos
- 备注：
- Nie, H., Yang, J., Zhou, G., Liu, C., Zheng, J., Zhang, W. X., Zhao, Y. J., Wang, H., & Wu, Y. (2017). Geochemical and Re–Os isotope constraints on the origin and age of the Songshugou peridotite massif in the Qinling orogen, central China. Lithos, 292–293, 307–319
- 上一条：Ordovician and Triassic mafic dykes in the Wudang terrane: Evidence for opening and closure of the South Qinling ocean basin, central China
- 下一条：Precambrian tectonothermal evolution of South Qinling and its affinity to the Yangtze Block: Evidence from zircon ages and Hf-Nd isotopic compositions of basement rocks