Crossmark

Grain boundary sliding as a formation mechanism for the crystal preferred orientation of antigorite: the formation and development of B-type antigorite CPO patterns

Crossref DOI link: https://doi.org/10.1186/s40645-025-00790-8

Published Online: 2026-01-21

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

Authors

Nagaya, Takayoshi https://orcid.org/0000-0001-7431-4828
Wallis, Simon R. https://orcid.org/0000-0002-7875-5740
Funding

Funding for this research was provided by:

Japan Society for the Promotion of Science (20K14575)

Japan Society for the Promotion of Science (20KK0079)

Japan Society for the Promotion of Science (24K07187)

Japan Society for the Promotion of Science (21H05202)
License Information

Text and Data Mining valid from 2026-01-21

Version of Record valid from 2026-01-21
More Information

Article History

Received: 8 September 2025

Accepted: 12 December 2025

First Online: 21 January 2026

Declarations

:

: The authors declare that they have no competing interest.

Document is current

Any future updates will be listed below