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Figure 2
X-ray diffraction results close to and after reaching constant hydrothermal conditions at 466 K and 1.35 MPa (230 min). The tobermorite 110 reflection intensity increases as the quartz 101 reflection intensity decreases. Fluorite serves as internal standard. (See Fig. S2 in the supporting information for the full range.)

Journal logoJOURNAL OF
APPLIED
CRYSTALLOGRAPHY
ISSN: 1600-5767
Volume 53| Part 4| August 2020| Pages 1163-1166
https://doi.org/10.1107/S1600576720006019
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