Hydrous phases and water transport in the subducting slab

Reviews in Mineralogy and Geochemistry

Volumn 62, Issue , 2006, Pages 273-289

  Kawamoto, Tatsuhiko ^a  

^a KYOTO UNIVERSITY   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 33749649830     PISSN: 15296466     EISSN: None     Source Type: Book Series    
DOI: 10.2138/rmg.2006.62.12     Document Type: Article

References (90)

1. 2O. Contrib Mineral Petrol 142: 714-723
2. 3+ substitution on high-pressure stability. Am Mineral 88: 99-108
3. Bureau H, Keppler H (1999) Complete miscibility between silicate melts and hydrous fluids in the upper mantle; experimental evidence and geochemical implications. Earth Planet Sci Lett 165:187-196
4. Bureau H, Ménez B, Malavergne V, Somogyi A, Munoz M, Simionovici A, Massare D, Burchard M, Kubsky S, Shaw C (2004) In situ determination of Pb, Sr, Rb, Zr partitioning between hydrous melts and aqueous fluids at high pressure and temperature. Eos Trans. AGU Fall Meet. Suppl. V11C-05
5. Davies JH, Stevenson DJ (1992) Physical model of source region of subduction zone volcanics. J Geophys Res 97:2037-2070
6. Demouchy S, Deloule E, Frost DJ, Keppler H (2005) Pressure and temperature-dependence of water solubility in Fe-free wadsleyite. Am Mineral 90:1084-1091
7. Domanik KJ, Holloway JR (1996) The stability and compositions of phengitic muscovite and associated phases from 5.5 to 11 GPa: Implications for deeply subducted sediments. Geochim Cosmochim Acta 60:4133-4150
8. 17(OH). Geochem J 12:191-194
9. 2O release from the slab. Earth Planet Sci Lett 214:187-201
10. Frost DJ (1999) The stability of dense hydrous magnesium silicates in Earth's transition zone and lower mantle. In: Mantle Petrology; Field Observations and High-pressure Experimentation; a Tribute to Francis R. (Joe) Boyd. Fei Y, Bertka C, Mysen BO (eds) Geochemical Society, p 283-296
11. Fumagalli P, Stixrude L, Poli S, Snyder D (2001) The 10 Å phase: a high-pressure expandable sheet silicate stable during subduction of hydrated lithosphere. Earth Planet Sci Lett 186:125-141
12. Fumagalli P, Poli, S (2005) Experimentally determined phase relations in hydrous peridotites to 6.5 GPa and their consequences on the dynamics of subduction zones. J Petrol 46:555-578
13. Furukawa Y (1993) Magmatic processes under arcs and formation of the volcanic front. J Geophys Res 98: 8309-8319
14. Gill JB (1981) Orogenic Andesite and Plate Tectonics: Springer-Verlag
15. 7]: an analogue of sursassite. Eur J Mineral 12:935-945
16. 2O up to 15 GPa. Phys Earth Planet Inter 85:237-263
17. 4: a new water reservoir in the mantle transition region. Geophys Res Lett 22:117-120
18. Inoue T, Irifune T, Yurimoto H, Miyagi I (1998) Decomposition of K-amphibole at high pressures and implications for subduction zone volcanism. Phys Earth Planet Inter 107:221-231
19. Irifune T, Kubo N, Isshiki M, Yamasaki Y (1998) Phase transformations in serpentine and transportation of water into the lower mantle. Geophys. Res Lett 25:203-206
20. 4 and some geophysical implications. J Geophys Res 94:10,637-10,646
21. 2O and melting in subduction zones. Earth Planet Sci Lett 160:65-80
22. 2O. Earth Planet Sci Lett 227:57-71
23. Kanzaki M, Kurita K, Fujii T, Kato T, Shimomura O, Akimoto S (1987) A new technique to measure the viscosity and density of silicate melts at high pressure. In: High-Pressure Research in Mineral Physics. Manghnani MH, Syono Y (eds) Ann Geophys Union, p 195-200
24. Kanzaki M (1991) Stability of hydrous magnesium silicates in the mantle transition zone. Phys Earth Planet Inter 66:307-312
25. 4 at high pressures and temperatures: precise determination of stabilities of olivine, modified spinel, and spinel. J Geophys Res 94:15,663-15,670
26. Kawamoto T, Hervig RL, Holloway JR (1996) Experimental evidence for a hydrous transition zone of the early Earth's mantle. Earth Planet Sci Lett 142:587-592
27. 2O-saturated mantle peridotite to 11 gigapascal. Science 276:240-243
28. 2O-saturated KLB-1 peridotite up to the uppermost lower mantle conditions. Phys Earth Planet Inter 143-144:387-395
29. Kawamoto T (2004b) Critical phenomena between magmas and aqueous fluid (in Japanese with English abstract). Rev High Press Sci Tech 14:235-241
30. 2O system. Am Mineral 89:1433-1437
31. 2O. Am J Sci 260:501-521
32. Kessel R, Ulmer P, Pettke T, Schmidt MW, Thompson AB (2005) The water-basalt system at 4 to 6 GPa: Phase relations and second critical endpoint in a K-free eclogite at 700 to 1400 °C. Earth Planet Sci Lett 237: 873-892
33. 4. Contrib Mineral Petrol 123:345-357
34. 2O up to 30 GPa, 1600 °C: Applications to hydrous peridotite subducting into the Earth's deep interior. J Geophys Res 109, doi: 10.1029/2003JB002651
35. Komabayashi T, Hirose K, Funakoshi K-i, Takafuji N (2005) Stability of phase A in antigorite (serpentine) composition determined by in-situ X-ray pressure observations. Phys Earth Planet Inter 151:276-289
36. 4: Possible hydrous magnesium silicate in the mantle transition zone. Phys Chem Minerals 23:461-469
37. 2O system up to 25 GPa. Phys Earth Planet Inter 134:105-127
38. Litasov K, Ohtani E (2005) Phase relations in hydrous MORB at 18-28 GPa: implications for heterogeneity of the lower mantle. Phys Earth Planet Inter 150:239-263
39. 2O on the phase behaviour of the forsterite - enstatite system at high pressures and temperatures and implications for the Earth. Phys Earth Planet Inter 49:142-167
40. Manning CE (2004) The chemistry of subduction-zone fluids. Earth Planet Sci Lett 223:1-16
41. Mibe K, Fujii T, Yasuda A (1998) Connectivity of aqueous fluid in the Earth's upper mantle. Geophy Res Lett 25:1233-1236
42. Mibe K, Fujii T, Yasuda A (1999) Control of the location of the volcanic front by aqueous fluid connectivity in the mantle wedge. Nature 401:259-262
43. Mibe K, Fujii T, Yasuda A (2002) Composition of aqueous fluid coexisting with mantle minerals at high pressure and its bearing on the differentiation of the Earth's mantle. Geochim Cosmochim Acta 66:2273-2285
44. Mibe K, Yoshino T, Ono S, Yasuda A, Fujii T (2003) Connectivity of aqueous fluid in eclogite and its implications for fluid migration in the Earth's interior. J Geophys Res 108, doi: 10.1029/2002JB001960
45. 2O system and its bearing on the magmatism in subduction zones. AGU Fall meeting (abstract), V11C-07
46. 2O systems using high pressure and high-temperature X-ray radiography. Geochim Cosmochim Acta 68:5189-5195
47. 2O system. AGU Fall meeting (abstract), V33C-03
48. 2O system. (in prep.)
49. 2O at 15 kbar. Carnegie Inst Wash Yearb 73:255-258
50. 2- saturated magmas in the island arc environment. J Geol 81:285-300
51. Niida K, Green DH (1999) Stability and chemical compositions of pargasitic amphibole in MORB pyrolite under mantle conditions. Contrib Mineral Petrol 135:18-40
52. Ohtani E, Toma M, Litasov K, Kubo T, Suzuki A (2001) Stability of dense hydrous magnesium silicate phases and water storage capacity in the transition zone and lower mantle. Phys Earth Planet Inter 124:105-117
53. Ono S (1998) Stability limits of hydrous minerals in sediment and mid-ocean ridge basalt compositions: implications for water transport in subduction zones. J Geophys Res 103:18253-18267
54. Ono S (1999) Water in the Earth's mantle (in Japanese with English abstract). Rev High Press Sci Tech 9:3-10
55. 2O fluid: implications for water transport by subducted oceanic crust. Earth Planet Sci Lett 203:895-903
56. 2O phase relationships and critical behavior at high pressures. Contrib Mineral Petrol 112:490-500
57. 2O recycling in subduction zones. Stability of lawsonite to 100 kbars. Contrib Mineral Petrol 118:99-108
58. 2O. Contrib Mineral Petrol 144:449-456
59. Pawley AR, Holloway JR (1993) Water sources for subduction zone volcanism: New experimental constraints. Science 260:664-667
60. 2O in subduction zones. Am Mineral 80:998-1003
61. Peacock SM (1993) Large-scale hydration of the lithosphere above subducting slabs. Chem Geol 108:49-59
62. Peacock SM, Wang K (1999) Seismic consequences of warm versus cool subduction metamorphism: examples from Southwest and Northeast Japan. Science 286:937-939
63. Poli S, Schmidt MW (1995) Water transport and release in subduction zones: experimental constraints on basaltic and andesitic systems. J Geophys Res 100:22299-22314
64. Ringwood AE, Major A (1967) Some high-pressure transformations of geophysical interest. Earth Planet Sci Lett 2:106-110
65. Ryabchikov ID, Schreyer W, Abraham K (1982) Compositions of aqueous fluid in equilibrium with pyroxenes and olivines at mantle pressures and temperatures. Contrib Mineral Petrol 79:80-84
66. Sakuyama M, Nesbitt RW (1986) Geochemistry of the Quaternary volcanic rocks of the northeast Japan arc. J Volcanol Geotherm Res 29:413-450
67. Schmidt M, Poli S (1998) Experimentally based water budgets for dehydrating slabs and consequences for arc magma generations. Earth Planet Sci Lett 163:361-379
68. Schmidt MW, Vielzeuf D, Auzanneau E (2004) Melting and dissolution of subducting crust at high pressures: the key role of white mica. Earth Planet Sci Lett 228:65-84
69. 2O system. Nature 385: 710-712
70. 4: a potential host for water in the mantle? Am Mineral 72:1051-1055
71. Smyth JR, Kawamoto T (1997) Hydrous wadsleyite II: A new, dense, high pressure, hydrous magnesium iron silicate phase. Earth Planet Sci Lett 146:E9-E16
72. 4). Am Mineral 82:270-275
73. 2O system. Contrib Mineral Petrol 143:32-37
74. 2O. Am Mineral 85:68-77
75. Stalder R, Ulmer P (2001) Phase relations of a serpentine composition between 5 and 14 GPa: significance of clinohumite and phase E as water carriers into the transition zone. Contrib Mineral Petrol 140:670-679
76. 2O under upper mantle conditions. Contrib Mineral Petrol 140:607-618
77. Sudo A, Tatsumi Y (1990) Phlogopite and K-amphibole in the upper mantle: Implication for magma generation in subduction zones. Geophys Res Lett 17:29-32
78. Suzuki A, Ohtani E, Kamada T (2000) A new hydrous phase delta-AlOOH synthesized at 20.9 GPa and 1000 °C. Phys Chem Mineral 27:689-693
79. Takei Y, Shimizu I (2003) The effects of liquid composition, temperature, and pressure on the equilibrium dihedral angles of binary solid - liquid systems inferred from a lattice-like model. Phys Earth Planet Inter 139:225-42
80. Tatsumi Y (1986) Formation of the volcanic front in subduction zones. Geophys Res Lett 13:717-720
81. Tatsumi Y (1989) Migration of fluid phases and genesis of basalt magmas in subduction zones. J Geophys Res 94:4697-4707
82. Tatsumi Y, Eggins S (1995) Subduction zone magmatism. Blackwell Science
83. Trønnes RG, Takahashi E, Scarfe CM (1988) Stability of K-richterite and phlogopite to 14 GPa. Trans Am Geophys Union 69:1510-1511
84. Ulmer P, Trommsdorff V (1995) Serpentine stability to mantle depths and subduction-related magmatism. Science 268:858-861
85. 2O fluids and their implications for fluid transport, host-rock physical properties, and fluid inclusion formation. Earth Planet Sci Lett 85:497-515
86. Watson EB, Brenan JM, Baker DR (1990) Distribution of fluids in the continental mantle. In: Continental Mantle. Menzies MA (ed) Oxford University Press, p 111-125
87. 2O at high pressures and temperatures - stability field for hydroxyl-chondrodite, hydroxyl-clinohumite and 10 Å -phase. Am J Sci 277:288-312
88. Zhang YG, Frantz JD (2000) Enstatite-forsterite-water equilibria at elevated temperatures and pressures. Am Mineral 85:918-925
89. 2O (ASH). Eur J Mineral 5:637-649
90. 2: A fully hydrated analogue of topaz. Am Mineral 78:285-297