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. 2020 Jun 9;11:2913. doi: 10.1038/s41467-020-16528-7

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© The Author(s) 2020

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Fig. 2 — Examples of disaggregation (a–c) and linear through-going fractures (d–f) in boulders of varying size. The orientation of linear fractures are in the (d) WNW-ESE and (e, f) N–S directions.