Ordovician and Triassic mafic dykes in the Wudang terrane: Evidence for opening and closure of the South Qinling ocean basin, central China.

MLA

Nie, Hu, et al. “Ordovician and Triassic Mafic Dykes in the Wudang Terrane: Evidence for Opening and Closure of the South Qinling Ocean Basin, Central China.” Lithos, vol. 266–267, Dec. 2016, pp. 1–15. EBSCOhost, https://doi.org/10.1016/j.lithos.2016.10.009.

APA

Nie, H., Wan, X., Zhang, H., He, J.-F., Hou, Z.-H., Siebel, W., & Chen, F. (2016). Ordovician and Triassic mafic dykes in the Wudang terrane: Evidence for opening and closure of the South Qinling ocean basin, central China. Lithos, 266–267, 1–15. https://doi.org/10.1016/j.lithos.2016.10.009

Chicago

Nie, Hu, Xin Wan, He Zhang, Jian-Feng He, Zhen-Hui Hou, Wolfgang Siebel, and Fukun Chen. 2016. “Ordovician and Triassic Mafic Dykes in the Wudang Terrane: Evidence for Opening and Closure of the South Qinling Ocean Basin, Central China.” Lithos 266–267 (December): 1–15. doi:10.1016/j.lithos.2016.10.009.