Reaction-induced fracturing during the hydration of the oceanic crust
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https://b2find.eudat.eu/dataset/b2e93cc2-253b-534c-9318-5a1f3e16cd90
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Near mid-oceanic ridges, microseismicity develops in large volumes of the oceanic crust and is interpreted to result from the hydration of oceanic rocks with a solid volume...
