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GEOPHYSICAL RESEARCH LETTERS
Volume 35, Issue 3, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2007GL031718
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In-situ X-ray diffraction experiments were conducted to determine the stability field of the aluminous hydrous mineral delta-AlOOH over the entire conditions of the lower mantle. We observed delta-AlOOH at pressures from 33 to 134 GPa at 1350-2300 K, indicating that this hydrous mineral in the sediment layer of a subducting slab could transport hydrogen into the core-mantle boundary (CMB).
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