Microstructures of olivine gabbros from the Atlantis Bank OCC (57°E Southwest Indian Ridge) reveal compaction-driven melts extraction and accumulation in ultraslow-spread oceanic crust. | Zendy

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Microstructures of olivine gabbros from the Atlantis Bank OCC (57°E Southwest Indian Ridge) reveal compaction-driven melts extraction and accumulation in ultraslow-spread oceanic crust.

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