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Revealing deformation mechanisms of the mineral antigorite in subduction zones

  • February 6, 2026 at 5:56 PM
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Revealing deformation mechanisms of the mineral antigorite in subduction zones
Earth's surface is covered by more than a dozen tectonic plates, and in subduction zones around the world—including the Japanese Islands—plates converge and dense oceanic plates sink into Earth's interior. These regions, especially plate boundaries, are known for frequent seismic activity.

Originally published at Phys.org

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