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The so-called "fore-arc basalts" were formed along short-lived spreading ridges, far and out of the influence of the Pacific subduction, until the slab's crust reached the depth of dehydration, favoring the eruption of the boninites.
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Shiina et al. (2013) showed the existence of free water in the crust at depths of 60 to 90 km beneath northeastern Japan, which is consistent with depths of dehydration reactions of hydrous minerals (Abers et al. 2013) and concentrated seismicity in the crust (Kita et al. 2006).
A seismic low-velocity layer in the slab crust persists down to the depth of this upper-plane seismic belt, which provides evidence for phase transformation of dehydration at this depth.
The difference in slab depth must produce the difference in the nature of dehydration from the subducting plate and the frictional property along the plate boundary.
The deepest drillhole into the igneous oceanic crust (ODP Site 504B; Alt et al. 1996) contains discrete saponite to a depth of ~600 m from the top of the basement material that is capable of dehydration.
The depth and shape of the 3-μm bands are correlated with the heating stage because of dehydration by heating.
This mechanism of dehydration embrittlement would certainly apply at pressures below c. 0.5 GPa (corresponding to c. 15 km depth).
They are dying of dehydration.
These changes increase the risk of dehydration.
· Drink plenty of fluids to avoid symptoms of dehydration.
The spell of dehydration had made him watchful.
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