Articles | Volume 38, issue 2
https://doi.org/10.5194/ejm-38-179-2026
https://doi.org/10.5194/ejm-38-179-2026
Research article
 | 
09 Apr 2026
Research article |  | 09 Apr 2026

Hydrous partial melting in gabbros drilled at the Southwest Indian Ridge (ODP Hole 735B): evidence from microstructures at grain boundaries

Jürgen Koepke

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Short summary
Gabbroic rocks from the Southwest Indian Ridge have been investigated. The results show that hydrous partial melting triggered by hydrothermal fluids percolating on grain boundaries above the wet gabbro solidus is a common process at slow-spreading mid-ocean ridges. The main indication of this process is plagioclase strongly enriched in anorthite content at grain boundaries, which can only be identified via backscattered electron imaging and related electron microprobe profiles.
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