Symmetry Breakdown in Franckeite: Spontaneous Strain, Rippling, and Interlayer Moiré

Riccardo Frisenda1, Gabriel Sanchez-Santolino1, Nikos Papadopoulos2

  • 1Materials Science Factory , Instituto de Ciencia de Materiales de Madrid (ICMM-CSIC) , Campus de Cantoblanco, Madrid 28049 , Spain.

Nano Letters
|January 14, 2020
PubMed
Summary

Franckeite is a mineral with alternating layers of SnS₂ and PbS structures. Despite these layers being isotropic, the mineral shows structural anisotropy due to spontaneous rippling. This rippling is linked to inhomogeneous strain and anisotropic electrical, vibrational, and optical properties. The study suggests that the incommensurability between the layers modulates van der Waals forces, leading to the observed symmetry breakdown. These findings may help understand similar phenomena in other layered materials.

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