Tuite, γ-Ca3( PO4)2, formed by chlorapatite decomposition in a shock vein of the Suizhou L6 chondrite.

MLA

Xie, Xiande, et al. “Tuite, γ-Ca3( PO4)2, Formed by Chlorapatite Decomposition in a Shock Vein of the Suizhou L6 Chondrite.” Meteoritics & Planetary Science, vol. 48, no. 8, Aug. 2013, pp. 1515–23. EBSCOhost, https://doi.org/10.1111/maps.12143.

APA

Xie, X., Zhai, S., Chen, M., & Yang, H. (2013). Tuite, γ-Ca3( PO4)2, formed by chlorapatite decomposition in a shock vein of the Suizhou L6 chondrite. Meteoritics & Planetary Science, 48(8), 1515–1523. https://doi.org/10.1111/maps.12143

Chicago

Xie, Xiande, Shuangmeng Zhai, Ming Chen, and Hexiong Yang. 2013. “Tuite, γ-Ca3( PO4)2, Formed by Chlorapatite Decomposition in a Shock Vein of the Suizhou L6 Chondrite.” Meteoritics & Planetary Science 48 (8): 1515–23. doi:10.1111/maps.12143.