Cite
40Ar/39Ar age of the onset of high-Ti phase of the Emeishan volcanism strengthens the link with the end-Guadalupian mass extinction.
MLA
Li, Youjuan, et al. “40Ar/39Ar Age of the Onset of High-Ti Phase of the Emeishan Volcanism Strengthens the Link with the End-Guadalupian Mass Extinction.” International Geology Review, vol. 60, no. 15, Nov. 2018, pp. 1906–17. EBSCOhost, https://doi.org/10.1080/00206814.2017.1405748.
APA
Li, Y., He, H., Ivanov, A. V., Demonterova, E. I., Pan, Y., Deng, C., Zheng, D., & Zhu, R. (2018). 40Ar/39Ar age of the onset of high-Ti phase of the Emeishan volcanism strengthens the link with the end-Guadalupian mass extinction. International Geology Review, 60(15), 1906–1917. https://doi.org/10.1080/00206814.2017.1405748
Chicago
Li, Youjuan, Huaiyu He, Alexei V. Ivanov, Elena I. Demonterova, Yongxin Pan, Chenglong Deng, Dewen Zheng, and Rixiang Zhu. 2018. “40Ar/39Ar Age of the Onset of High-Ti Phase of the Emeishan Volcanism Strengthens the Link with the End-Guadalupian Mass Extinction.” International Geology Review 60 (15): 1906–17. doi:10.1080/00206814.2017.1405748.