Stability field of new hydrous phase, δ-AIOOH, with implications for water transport into the deep mantle

Geophysical Research Letters

Volumn 28, Issue 20, 2001, Pages 3991-3993

  Ohtani, Eiji ^a   Litasov, Konstantin ^a   Suzuki, Akio ^a   Kondo, Tadashi ^a  

^a TOHOKU UNIVERSITY   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

MAGNESIUM PRINTING PLATES; RESERVOIRS (WATER); SILICON; EARTH SCIENCES; GEOPHYSICS;

HYDROUS PHASES;

GEOPHYSICS; RESERVOIRS (WATER);

CRYSTAL CHEMISTRY; HYDROUS MINERAL; LOWER MANTLE; MINERALOGY; WATER;

DEEP MANTLES; HIGH-PRESSURE POLYMORPH; HYDROUS PHASE; LOWER MANTLE; OCTAHEDRALLY COORDINATED; SUBDUCTING SLABS; WATER TRANSPORT;

EID: 0035888469     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2001GL013397     Document Type: Article

References (21)

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5. 4 and some geophysical implications
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7. A new device for high pressure vessels
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9. 4 determined by in Situ X-ray observation
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13. 3(OH)
14. Hydrogen in stishovite, with implications for mantle water content
15. Lawsonite: Upper pressure stability and formation of higher density hydrous phases
16. Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation
17. 3OH, a high-pressure hydrous phase
18. A new hydrous phase δ- AIOOH sysnthesized at 20.9 GPa and 1000°C
19. A new post-stishovite high-pressure polymorph of silica
20. 2O (ASH)
21. 2: A fully hydrated analogue of topaz