Cite
The role of water in the structures of synthetic hallimondite, Pb2[(UO2)(AsO4)2](H2O)n and synthetic parsonsite, Pb2[(UO2)(PO4)2](H2O)n, 0 ≤ n ≤ 0.5.
MLA
Locock, Andrew J., et al. “The Role of Water in the Structures of Synthetic Hallimondite, Pb2[(UO2)(AsO4)2](H2O)n and Synthetic Parsonsite, Pb2[(UO2)(PO4)2](H2O)n, 0 ≤ n ≤ 0.5.” American Mineralogist, vol. 90, no. 1, Jan. 2005, pp. 240–46. EBSCOhost, https://doi.org/10.2138/am.2005.1705.
APA
Locock, A. J., Burns, P. C., & Flynn, T. M. (2005). The role of water in the structures of synthetic hallimondite, Pb2[(UO2)(AsO4)2](H2O)n and synthetic parsonsite, Pb2[(UO2)(PO4)2](H2O)n, 0 ≤ n ≤ 0.5. American Mineralogist, 90(1), 240–246. https://doi.org/10.2138/am.2005.1705
Chicago
Locock, Andrew J., Peter C. Burns, and Theodore M. Flynn. 2005. “The Role of Water in the Structures of Synthetic Hallimondite, Pb2[(UO2)(AsO4)2](H2O)n and Synthetic Parsonsite, Pb2[(UO2)(PO4)2](H2O)n, 0 ≤ n ≤ 0.5.” American Mineralogist 90 (1): 240–46. doi:10.2138/am.2005.1705.