Cite
Zircon U–Pb–Hf isotopes and bulk-rock geochemistry of gneissic granites in the northern Jiamusi Massif, Central Asian Orogenic Belt: implications for Middle Permian collisional orogeny and Mesoproterozoic crustal evolution.
MLA
Cui, Pei-Long, et al. “Zircon U–Pb–Hf Isotopes and Bulk-Rock Geochemistry of Gneissic Granites in the Northern Jiamusi Massif, Central Asian Orogenic Belt: Implications for Middle Permian Collisional Orogeny and Mesoproterozoic Crustal Evolution.” International Geology Review, vol. 55, no. 9, July 2013, pp. 1109–25. EBSCOhost, https://doi.org/10.1080/00206814.2013.767489.
APA
Cui, P.-L., Sun, J.-G., Han, S.-J., Zhang, P., Zhang, Y., Bai, L.-A., & Gu, A.-L. (2013). Zircon U–Pb–Hf isotopes and bulk-rock geochemistry of gneissic granites in the northern Jiamusi Massif, Central Asian Orogenic Belt: implications for Middle Permian collisional orogeny and Mesoproterozoic crustal evolution. International Geology Review, 55(9), 1109–1125. https://doi.org/10.1080/00206814.2013.767489
Chicago
Cui, Pei-Long, Jing-Gui Sun, Shi-Jiong Han, Peng Zhang, Yong Zhang, Ling-An Bai, and A-Lei Gu. 2013. “Zircon U–Pb–Hf Isotopes and Bulk-Rock Geochemistry of Gneissic Granites in the Northern Jiamusi Massif, Central Asian Orogenic Belt: Implications for Middle Permian Collisional Orogeny and Mesoproterozoic Crustal Evolution.” International Geology Review 55 (9): 1109–25. doi:10.1080/00206814.2013.767489.