Cite
Neoproterozoic intraplate crustal accretion on the northern margin of the Yangtze Block: Evidence from geochemistry, zircon SHRIMP U–Pb dating and Hf isotopes from the Fuchashan Complex.
MLA
Liu, Lei, et al. “Neoproterozoic Intraplate Crustal Accretion on the Northern Margin of the Yangtze Block: Evidence from Geochemistry, Zircon SHRIMP U–Pb Dating and Hf Isotopes from the Fuchashan Complex.” Precambrian Research, vol. 268, Oct. 2015, pp. 97–114. EBSCOhost, https://doi.org/10.1016/j.precamres.2015.07.004.
APA
Liu, L., Yang, X., Santosh, M., Aulbach, S., Zhou, H., Geng, J., & Sun, W. (2015). Neoproterozoic intraplate crustal accretion on the northern margin of the Yangtze Block: Evidence from geochemistry, zircon SHRIMP U–Pb dating and Hf isotopes from the Fuchashan Complex. Precambrian Research, 268, 97–114. https://doi.org/10.1016/j.precamres.2015.07.004
Chicago
Liu, Lei, Xiaoyong Yang, M. Santosh, S. Aulbach, Hongying Zhou, Jianzhen Geng, and Weidong Sun. 2015. “Neoproterozoic Intraplate Crustal Accretion on the Northern Margin of the Yangtze Block: Evidence from Geochemistry, Zircon SHRIMP U–Pb Dating and Hf Isotopes from the Fuchashan Complex.” Precambrian Research 268 (October): 97–114. doi:10.1016/j.precamres.2015.07.004.