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The crystal structure of the new phase is very similar to that of CaCl<jats:sub>2</jats:sub>‐type SiO<jats:sub>2</jats:sub> and has monoclinic symmetry with space group <jats:italic>P2/m</jats:italic>. This new hydrous phase is stable up to about 52 GPa and then dissociates into MgSiO<jats:sub>3</jats:sub> perovskite and H<jats:sub>2</jats:sub>O (ice VIII) at static 0 K conditions. The Clapeyron slope between phase D and the new phase + SiO<jats:sub>2</jats:sub> is positive; about 6.4 MPa/K at 1000 K. This new hydrous phase further extends the stability field of dense hydrous magnesium silicates and also opens the pathway toward the existence of a high‐pressure phase of ice at the lower mantle conditions.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420001326216252416","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"00527608"},{"@type":"NRID","@value":"1000000527608"},{"@type":"NRID","@value":"9000002103225"},{"@type":"NRID","@value":"9000264242172"},{"@type":"NRID","@value":"9000001095654"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/7000014815"}],"foaf:name":[{"@value":"Jun Tsuchiya"}],"jpcoar:affiliationName":[{"@value":"Geodynamics Research Center Ehime University  Matsuyama Japan"},{"@value":"Earth‐Life Science Institute Ehime Satellite Ehime University  Matsuyama 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