Cite
Complex IR spectra of OH–groups in silicate glasses: Implications for the use of the 4500 cm–1IR peak as a marker of OH–groups concentration
MLA
Le Losq, Charles, et al. “Complex IR Spectra of OH–groups in Silicate Glasses: Implications for the Use of the 4500 Cm–1IR Peak as a Marker of OH–groups Concentration.” American Mineralogist (De Gruyter), vol. 100, no. 4, Apr. 2015, pp. 945–50. EBSCOhost, https://doi.org/10.2138/am-2015-5076.
APA
Le Losq, C., Cody, G. D., & Mysen, B. O. (2015). Complex IR spectra of OH–groups in silicate glasses: Implications for the use of the 4500 cm–1IR peak as a marker of OH–groups concentration. American Mineralogist (De Gruyter), 100(4), 945–950. https://doi.org/10.2138/am-2015-5076
Chicago
Le Losq, Charles, George D. Cody, and Bjorn O. Mysen. 2015. “Complex IR Spectra of OH–groups in Silicate Glasses: Implications for the Use of the 4500 Cm–1IR Peak as a Marker of OH–groups Concentration.” American Mineralogist (De Gruyter) 100 (4): 945–50. doi:10.2138/am-2015-5076.