A reply to comment on “An experimental study of symmetry lowering of analcime”

Abstract

The fracture surfaces of analcimes reported by Sugano and Kyono (Phys Chem Miner, 2018) were re-investigated using field-emission scanning electron microscopy. The results of scanning electron microscopic observation show the fractures can be characterized by smoothly curved surfaces, called sub-conchoidal fracture, and neither the lamellar twin nor the domain walls of twin were found on the surfaces of the analcimes. In addition, the lamellar twin is generally formed by transformation from the high-temperature phase or from pseudomorphic replacement under strong alkaline conditions. Actually, the symmetry lowering of analcime reported by Sugano and Kyono (2018) occurs at 200 °C. The temperature is much lower than the transformation from the high-temperature phase. In the hydrothermal experiment (Sugano and Kyono 2018), moreover, the analcimes were synthesized under acidic condition and reheated in pure water. No twin domain is likely to be formed under the hydrothermal condition. These facts strongly deny the possibility that the twin domains cause the pseudo-symmetry of tetragonal analcime. Consequently, it can be concluded that the observed forbidden reflections for the cubic Ia3d symmetry are not due to the presence of twin domains, but due to the symmetry lowering of analcime from cubic Ia3d to orthorhombic Ibca.

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Correspondence to Atsushi Kyono.

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Figure S1

(A) The lamellar twin texture of analcime covered on the surface reported by Xia et al. (2009). Fracture surfaces of analcime single crystal (B) used as a starting material by Sugano and Kyono (2018), (C) reheated hydrothermally for 24 h, and (D) for 48 h. Scale bar = 10 μm (TIF 678 KB)

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Kyono, A. A reply to comment on “An experimental study of symmetry lowering of analcime”. Phys Chem Minerals 45, 395–396 (2018). https://doi.org/10.1007/s00269-018-0952-3

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Keywords

  • Analcime
  • Hydrothermal treatment
  • SEM
  • Fracture surface