A single crystal of a-Ca 2 [HSiO 4 ](OH) (a-C 2 SH) was repeatedly imaged at room temperature with synchrotron mid-infrared microscopy after heating to 310°C, 340°C, 370°C, and 400°C respectively. The mechanisms of the observed phase transformations are discussed on the basis of a modular concept of the crystal structures. All images show domains of dellaite, Ca 6 [Si 2 O 7 ][SiO 4 ](OH) 2 , which are predominantly formed in the core of the crystal. In the crystal rim area a-C 2 SH persists in higher abundance. The mechanism of the phase transformation of a-C 2 SH into dellaite includes the following: (1) O. We suggest that reaction (1) cannot be completed at ambient pressure. Thus in the regions close to the rim of the crystals we expect the formation of x-C 2 S, which starts along the crystal edges according to Ca 2 [HSiO 4 ](OH) ? Ca 2 SiO 4 + H 2 O. Based on a modular concept, a structural relationship between a-C 2 SH, killalaite, dellaite, and x-C 2 S has been established. Similarities and differences in the thermal behavior of a-C 2 SH and afwillite have been highlighted.