Cite
Paleo- to Eoarchean crustal evolution in eastern Hebei, North China Craton: New evidence from SHRIMP U–Pb dating and in-situ Hf isotopic study of detrital zircons from paragneisses.
MLA
Liu, Shoujie, et al. “Paleo- to Eoarchean Crustal Evolution in Eastern Hebei, North China Craton: New Evidence from SHRIMP U–Pb Dating and in-Situ Hf Isotopic Study of Detrital Zircons from Paragneisses.” Journal of Asian Earth Sciences, vol. 78, Dec. 2013, pp. 4–17. EBSCOhost, https://doi.org/10.1016/j.jseaes.2013.07.041.
APA
Liu, S., Wan, Y., Sun, H., Nutman, A. P., Xie, H., Dong, C., Ma, M., Liu, D., & Jahn, B. (2013). Paleo- to Eoarchean crustal evolution in eastern Hebei, North China Craton: New evidence from SHRIMP U–Pb dating and in-situ Hf isotopic study of detrital zircons from paragneisses. Journal of Asian Earth Sciences, 78, 4–17. https://doi.org/10.1016/j.jseaes.2013.07.041
Chicago
Liu, Shoujie, Yusheng Wan, Huiyi Sun, Allen P. Nutman, Hangqiang Xie, Chunyan Dong, Mingzhu Ma, Dunyi Liu, and Bor-ming Jahn. 2013. “Paleo- to Eoarchean Crustal Evolution in Eastern Hebei, North China Craton: New Evidence from SHRIMP U–Pb Dating and in-Situ Hf Isotopic Study of Detrital Zircons from Paragneisses.” Journal of Asian Earth Sciences 78 (December): 4–17. doi:10.1016/j.jseaes.2013.07.041.