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The equilibrium between aqueous fluids and allanite-bearing eclogite has been investigated to constrain the effect of temperature (T) and fluid composition on the stability of allanite and on the mobility of major and trace elements during the dehydration of eclogites. The experiments were performed at 590–800°C and 2.4–2.6GPa, and fluids were sampled as synthetic fluid inclusions in quartz using...
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