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. 2019 Nov 12;10:5129. doi: 10.1038/s41467-019-12882-3

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© The Author(s) 2019

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 3 — Comparison of different projections of IWW and IPC-18. C_s-corrected STEM-ADF images of IWW (a, b) and IPC-18 (c, d) zeolites: a, c—top [100] view of the layers, which remain intact during the VPT rearrangement (crystallographic models of the same layer are superimposed for clarity), b, d—side [010] view showing the decrease in interlayer distance caused by the transformation of D4Rs into S4Rs