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The H2O component of sheared mantle peridotites from the Kaapvaal craton: evidence for hydrous deformation with implications for the stability of cratons

Crossref DOI link: https://doi.org/10.1007/s00410-025-02295-5

Published Online: 2026-01-24

Published Print: 2026-02

Update policy: https://doi.org/10.1007/springer_crossmark_policy

Authors

Heckel, Catharina https://orcid.org/0000-0002-0890-7876
Withers, Anthony C.

Woodland, Alan B.

Gibson, Sally A.

Ludwig, Thomas
Funding

Funding for this research was provided by:

Johann Wolfgang Goethe-Universität, Frankfurt am Main
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Article History

Received: 8 September 2025

Accepted: 30 December 2025

First Online: 24 January 2026

Declarations

:

: The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

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