Abstract
Phase transformations are widely invoked as a source of rheological weakening during subduction, continental collision, mantle convection and various other geodynamic phenomena. However, despite more than half a century of research, the likelihood and magnitude of such weakening in nature remain poorly constrained. Here we use experiments performed on a synchrotron beamline to reveal transient weakening of up to three orders of magnitude during the polymorphic quartz to coesite (SiO2) and olivine to ringwoodite (Fe2SiO4) phase transitions. Weakening becomes increasingly prominent as the transformation outpaces deformation. We suggest that this behaviour is broadly applicable among silicate minerals undergoing first-order phase transitions and examine the likelihood of weakening due to the olivine-spinel, (Mg,Fe)2SiO4, transformation during subduction. Modelling suggests that cold, wet slabs are most susceptible to transformational weakening, consistent with geophysical observations of slab stagnation in the mantle transition zone beneath the western Pacific. Our study highlights the importance of incorporating transformational weakening into geodynamic simulations and provides a quantitative basis for doing so.
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Data availability
The stress, strain and phase proportion measurements for each experimental run provided in Supplementary Data 1 and Supplementary Videos 1–14 are also publicly available via Figshare at https://doi.org/10.6084/m9.figshare.28726712 (ref. 50).
Code availability
The MATLAB code used for the slab weakening model is provided in Supplementary Code 1 and is also publicly available via Figshare at https://doi.org/10.6084/m9.figshare.28726712 (ref. 50).
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Acknowledgements
We thank L. Tokle and A. Dillman for providing the quartz and olivine starting materials, respectively. This work was funded through National Science Foundation (NSF) awards EAR-2023128 (to A.J.C.), EAR-2003389 (to A.J.C.), EAR-2023058 (to D.L.G.), EAR-2023061 (to L.N.H.) and EAR-1806791 (to K.M.K.). D.W. was supported by a UK Research and Innovation Future Leaders Fellowship, MR/V021788/1. A.J.C. acknowledges additional salary support from the Investment in Science Program (ISP) and Assistant Scientist Endowment Support (ASES) programmes at Woods Hole Oceanographic Institution (WHOI). Use of the Advanced Photon Source, Argonne National Laboratory, was supported by the US Department of Energy, Office of Science, Office of Basic Energy Sciences, under contract number DE-AC02-06CH11357. Use of the 6-BM-B beamline was supported by COMPRES, the Consortium for Materials Properties Research in Earth Sciences, under NSF Cooperative Agreement EAR 16-06856. Portions of this work were performed under the auspices of the US Department of Energy by Lawrence Livermore National Laboratory under contract DE-AC52-07NA27344. LLNL-JRNL-859365.
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A.J.C. and D.L.G. conceived of the study. All authors helped to conduct the experiments. K.M.K., L.N.H. and A.J.C. wrote the code for processing the experiment data. A.J.C. performed all the data processing, analysis and modelling. A.J.C. wrote the paper, with review and editing provided by all authors.
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Nature Geoscience thanks Julien Gasc and the other, anonymous, reviewer(s) for their contribution to the peer review of this work. Primary Handling Editor: Alison Hunt, in collaboration with the Nature Geoscience team.
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Supplementary Information
Supplementary Figs. 1–11, Tables 1–3 and Text 1–4.
Supplementary Data 1
Mechanical data.
Supplementary Code 1
Slab model code.
Supplementary Video 1
Movie of experiment San467.
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Cross, A.J., Goddard, R.M., Kumamoto, K.M. et al. Direct observations of transient weakening during phase transformations in quartz and olivine. Nat. Geosci. 18, 548–554 (2025). https://doi.org/10.1038/s41561-025-01703-6
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DOI: https://doi.org/10.1038/s41561-025-01703-6


