Recent Progress in Experimental Mineral Physics: Phase Relations of Hydrous Systems and the Role of Water in Slab Dynamics

Earth's Deep Mantle: Structure, Composition, and Evolution

Volumn , Issue , 2013, Pages 321-334

  Ohtani, Eiji ^a  

^a TOHOKU UNIVERSITY   (Japan)

Author keywords

Earth Mantle Research; Heat Convection, Natural Research; Seismology Research; Thermochemistry Research

Indexed keywords

BIOLOGY; HEAT CONVECTION; PEROVSKITE; SEISMOLOGY; TECTONICS;

EARTH MANTLE; SEDIMENT LAYERS; SEISMIC REFLECTORS; SUBDUCTING SLABS; SUBDUCTION ZONES; TEMPERATURE PROFILES; TRANSITION ZONES; WATER STORAGE CAPACITY;

TRANSPORT PROPERTIES;

EID: 84951134544     PISSN: None     EISSN: None     Source Type: Book    
DOI: 10.1029/160GM19     Document Type: Chapter

References (104)

1. 12: transition boundaries with positive pressure-temperature slopes. Phys. Earth Planet. Inter. 114, 129-140. 416-422.
2. 12 at high pressures and high temperatures: phase equilibria, calorimetry and implications for mantle structure, Phys. Earth Planet. Inter., 132, 303-324, 2002.
3. Anderson, D. L., Theory of the Earth.Blackwell Scientific Publ., Boston, 366p, 1989.
4. Anderson, O. L., D. Isaak, H Oda, 1991. Thermoelastic parameters of six minerals at high temperatures. J. Geophys. Res. 96, 18037-18046, 1991.
5. Anderson, O. L., D. Isaak, H Oda, High-temperature elastic constant data on minerals relevant to geophysics. Rev. Geophys. 30, 57-90, 1992.
6. 20 system up to 24 GPa: implications for the distribution of water in the Earth's mantle, Earth Planet. Sci. Let. 182, 209-221, 2000.
7. Bolfan-Casanova N, S. Mackwell, H. Kepple., C. McCammon, D. C. Rubie, Pressure dependence of H solubility in magnesio-wustite up to 25 GPa: implications for the storage of water in the Earth's lower mantle, Geophys. Res. Lett., 10, 1029, 2002.
8. Bose, K. and J. Gangley, Experimental and theoretical studies of the stabilies of talc, antigolite, and phase A at high pressures with application to subduction processes, Earth Planet. Sci. Lett., 136, 109-121, 1994.
9. Carpenter, M. A., R. J. Hemley, H-K. Mao, High pressure elasticity of stishovite and the P42/mnm-Pnnm phase transition, Geophys. Res., 105, 10807-10816, 2000.
10. Collier, J. D., G. R. Helffrich, and B. J. Wood, Seismic discontinuities and subduction zones, Phys. Earth Planet. Inter., 127, 35-49, 2001.
11. Davies, J. H. and D. J. Stevenson, Physical model for the source region of subduction zone volatiles, J. Geophys. Res., 97, 2037-2070, 1992.
12. Dixon, J. E., L. Leist, C. Langmuir, J. G. Schilling, Recycled dehydrated lithosphère observed in plume-influenced mid-ocean-ridge basalt, Nature, 420, 385-389, 2002.
13. Domanik, K. and J. R. Holloway, The stability and composition of phengitic muscovite and associated phases from 5.5 to 11 GPa: implications for deeply subducted sediments, Geochim. Cosmochim. Acta, 60, 4233-4150, 1996.
14. Duffy, T. S., Ahrens, T. J., Compressional sound velocity, equation of state, and constitutive response of shock-compressed magnesium oxide. J. Geophys. Res. 100, 529-542, 1995.
15. 17(0H), Geochem. J., 12, 191-194, 1979.
16. Eshelby, D., The determination of the elastic field of an ellipsoidal inclusion, and related problem, Proc. Roy. Soc. London, Ser. A, 241, 376-396, 1957.
17. Evans, B. W., W. Johannes, H. Oterdoom, V. Trommsdorff, Stability of chrysotile and antigorite in their serpentine multisystem, Schweiz, Mineral. Petrogr. Mitt., 50, 481-492, 1976.
18. 3 perovskite as a function of temperature at 26 GPa: Implication for FeO content in the lower mantle. J. Geophys. Res., 101, 11525-11530, 1996.
19. 0.4)O. Phys. Chem. Minerals 18, 416-422, 1992.
20. 4 using MgO as an internal pressure standard and its geophysical implications: J. Geophys. Res., v. 109, doi: 10.1029/2003JB002562.
21. Frost D. J., C. Liebske, F. Langenhorst, C. McCammon, R. G. Tronnes, D. C. Rubie, Experimental evidence of iron-rich metal in the Earth's lower mantle, Nature, 428, 409-411, 2004.
22. Fukao, Y, S. Widiyantoro, M. Obayashi, Stagnant slabs in the upper and lower mantle transition region, Rev. Geophys., 39, 291-323, 2001.
23. Fumagalli P, L. Stixrude, S. Poli, and L. Snyder, The 10Å phase: a high pressure expandable sheet silicate during subduction of hydrated lithosphere, Earth Planet. Sci. Lett., 186, 125-141, 2001.
24. 3 perovskite determined by in situ X-ray observations up to 30 GPa and 2000 K, J. Geophys. Res. 101, 8257-8269, 1996.
25. Gasparik, T., Phase relations in the transition zone, J. Geophys. Res., 95, 15751-15769, 1990.
26. Hazen, R. M., R. T. Downs, L. W. Finger, and Ko, J. Crystal chemistry of ferromagnesian silicate spinels: evidence for Mg-Si disorder. Am. Mineral. 78, 1320-1323, 1993.
27. 12), and garnet symmetry in the earth's transition zone. Phys. Chem. Minerals 24, 206-221, 1997.
28. 4: A new water reservoir in the mantle transition region, Geophys. Res. Lett, 160, 117-120, 1995.
29. 4, Earth Planet. Sci. Lett., 160, 107-113, 1998.
30. 4 determined by in situ X-ray diffraction, Science 279 (1998) 1698-1700.
31. Ito, E., Yamada, H., Stability relations of silicate spinels, ilmenites, and perovskites. In: Akimoto, S., Manghnani, M. H. (Eds.), High-Pressure Research in Geophysics. Center for Academic Publication, Japan, pp. 405-419, 1982.
32. Jagoutz E, H. Palme,H. Baddenhausen, K. Blum, M. Cendales, G. Dreibus, B. Spettel, V. Lorenz, H. Wanke, The abundances of major, minor and trace elements in the Earth's mantle as derived from primitive ultramafic nodules. Proc 10th Lunar Planet Sci Conf, Tucson, Arizona, pp 2031-2050, 1979.
33. Kaneshima, S. and G. Helffrich, Detection of lower mantle scatterers northeast of the Mariana subduction zone using short-period array data, J. Geophys. Res., 103, 4825-4838, 1998.
34. Kaneshima, S. and G. Helffrich, Dipping lower-velocity layer in the mid-lower mantle: evidence for geochemical heterogeneity, Science, 283, 1888-1891, 1999.
35. Kaneshima, S. Small-scale heterogeneity at the top of the lower mantle around the Mariana slab, Earth Planet. Sci. Lett., 209, 85-101, 2003.
36. Kaneshima, S. and G. Helffrich, Subparallel dipping heterogeneities in the mid-lower mantle, J. Geophys. Res., 108, doi: 10.1029/2001jb001596, 2003.
37. Kanzaki, M., Stability of hydrous magnesium silicates in the mantle transition zone, Phys. Earth Planet. Inter., 66, 307-316, 1991.
38. 3 perovskite at lower mantle pressures. Geophys. Res. Lett. 25, 2741-2744. 5-24, 1998.
39. 4 determined by in situ X-ray diffractometry, Phys. Earth Planet. Inter, 136, 11-24, 2003.
40. 20-saturated KLB-1 peridotite up to 15 GPa, in Volatiles in the Earth and Solar System, edited by K. A. Farley, pp.229-239, Amer. Inst, of Phys., New York, 1995.
41. Kawamoto, T., R. L. Hervig, and R. Holloway, Experimental evidence for a hydrous transition zone in the Earth's early mantle, Earth Planet. Sci. Lett, 142, 587-592, 1996.
42. Kesson, S. and A. E. Ringwood. Slab-mantle interactions. I. Sheared and refertillised garnet peridotite xenoliths-samples of wadachi-benioff zone? Chem. Geol, 78, 83-96, 1989.
43. 4, Contrib. Mineral. Petrol, 123, 345-357, 1996.
44. Konzett, J. and Y. Fei, Hydrous potassic phases at high pressures: the stability of potassium amphibole and phase X and a new ordered hydrous pyribole, EOS Trans, Amer. Geophys. Union, 79 (17), S161, 1998.
45. Konzett, J. and P. Ulmer, The stability of hydrous potassic phases in lherzolitic mantle-an experimental study to 9.5 GPa in simplified and natural bulk compositions, Jour. Petrol., 40, 629-652, 1999.
46. Koper, K. D., D. A. Wiens, L. M. Dorman, J. A. Hildebrand, and S. C. Webb, Modeling the Tonga slab: can travel time data resolve a metastable olivine wedge? J. Geophys. Res. 103: 30079-30100, 1998.
47. Koyama, T, H. Shimizu, H. Utada, E. Ohtani, and R. Hae, Water content in the mantle transition zone beneath north Pacific derived from the electrical conductivity anomaly, Eos, 85 (47), Fall meeting suppl., abstract, T31F-05, 2004.
48. 12 up to 28 GPa: phase relations of garnet, ilmenite and perovskite. Phys. Earth Planet. Inter. 121, 85-102, 2000.
49. Kubo, T, E. Ohtani, T. Kato, T. Shinmei, and K. Fujino, Effect of water on the α-β transformation kinetics in San Carlos Olivine, Science, 281, 85-87, 1998.
50. Kubo, T, E. Ohtani, T. Kondo, T. Kato, M. Toma, T. Hosoya, A. Sano, T. Kikegawa, and T. Nagase, Metastable garnet in oceanic crust at the top of the lower mantle, Nature, 420, 803, 2002.
51. Kudoh Y, T. Nagase, H. Mizobata, E. Ohtani, S. Sasaki, and M. Tanaka, Structure and crystal chemistry of phase G, a new hydrous magnesium silicate synthesized at 22 GPa and 1050°C, Geophys. Res. Lett, 24, 1051-1054, 1997.
52. 3 perovskite: implications for seismic discontinuities in the lower mantle, Phys. Earth and Planet. Inter, 145, 67-74, 2004.
53. 20 system up to 25 GPa, Phys. Earth Planet. Inter., 134, 105-127, 2002.
54. 20 system up to 25 GPa, Phys. Chem. Minerals, 30, 147-156, 2003.
55. Litasov, K., E. Ohtani, A. Suzuki, T. Kawazoe, K. Funakoshi, Absence of density crossover between basalt and peridotite in the cold slabs passing through 660 km discontinuity, Geophys. Res. Lett, 31, L24607, doi:10.1029/2004GL21306, 2004.
56. Litasov, K. and E. Ohtani, Phase Relations in Hydrous MORB at 18-25 GPa: Implications for Heterogeneity of the Lower Mantle, Phys. Earth Planet. Inter, 150, 239-263, 2005.
57. Litasov K., E. Ohtani, F. Langenhorst, H. Yurimoto, T. Kubo, and T. Kondo, Water solubility in Mg-perovskites and water storage capacity in the lower mantle, Earth Planet. Sci. Lett., 211, 189-203, 2003.
58. Litasov, K., E. Ohtani, A. Sano, A. Suzuki, and K. Funakoshi, 2005, Wet Subduction versus Cold Subduction: Geophys. Res. Lett., 32, L13312, doi:10.1029/2005GL022921, 2005.
59. Luth, R. W., Is phase A relevant to the Earth's mantle, Geochim. Cosmochim. Acta, 59, 679-682, 1995.
60. Luth, R. W., Experimental study of the system phlogopite-diopside from 3.5 to 17 GPMm. Mineral., 82, 1198-1209, 1997.
61. Matsubara, R., H. Toraya, S. Tanaka, H. Sawamoto, Precision lattice parameter determination of (Mg, Fe)SiO3 tetragonal garnet, Science 247, 697-699, 1990.
62. MiyajimaN, K. Fujino, N. Funamori, T. Kodo, and T. Yagi, Garnet-perovskite transformation under conditions of the Earth's lower mantle: an analytical transmission electron microscopy study. Phys. Earth Planet. Inter, 116, 117-131, 1999.
63. Murakami M, K. Hirose, H. Yurimoto, S. Nakashima, and N. Taka-fuji, Water in Earth's lower mantle, Science 295, 1885-1887, 2002.
64. Niu F, H. Kawakatsu, and Y. Fukao, A slightly dipping and strong seismic reflector at the mid-mantle depth beneath the Mariana subduction zone, J. Geophys. Res., 108, 2419, doi:10.1029/ 2002JB002384, 2003.
65. Oguri, K., N. Funamori, T. Uchida, N. Miyajima, T. Yagi, and T. Fujino, Post-garnet transition in a natural pyrope: a multi-anvil study based on in situ X-ray diffraction and transmission electron microscopy, Phys. Earth Planet. Inter., 122, 175-186, 2000.
66. 20 at pressures up to 27 GPa, Phys. Chem. Minerals, 27, 533-544, 2000.
67. Ohtani, E., M. Toma, T. Kubo, and T. Kondo, T. Kikegawa, Geophys. Res. Lett, 30, 1029, doi:10.1029/2002GL015549, 2003.
68. Ohtani, E., K. Litasov, T. Hosaya, T. Kubo, and T. Kondo, Water transport into the deep mantle and formation of a hydrous transition zone, Phys. Earth Planet. Inter, 143-144, 201-213, 2004.
69. Ono, S., Stability limits of hydrous minerals in sediment and mid-ocean ridge basalt compositions: Implications for water transport in subduction zones, J. Geophys. Res., 103, 18253-18264, 1998.
70. 3(OH). Contrib. Mineral. Petrol, 137, 83-89, 1999.
71. Ono, S., K. Hirose, M. Isshiki, K. Mibe, Y. Saito, Equation of state of hexagonal aluminous phase in basaltic composition to 63 GPa at 300 K, Phys. Chem. Mineral, 29, 527-531, 2002.
72. 3 tetragonal garnet. Phys. Earth Planet. Inter. 99, 145-154, 1997.
73. 20 for subduction magmatism, Terra, 8, Abstr. Suppl.,1, 50, 1996.
74. Peacock, S. M., Fluid processes in subduction zone, Science, 248, 329-337, 1990.
75. Poli, S., The amphiborite-eclogite transformation: an experimental result on basalt, Am. J. Sci., 293, 1061-1107, 1993.
76. Poli, S and M. W. Schmidt, Petrology of subducted slabs, Ann. Rev. Earth Planet. Sci., 30, 207-235, 2002.
77. Revenaugh J and S. A. Sipkin, Seismic evidence for silicate melt atop the 410-km mantle discontinuity, Nature, 369, 474-476, 1994.
78. Rigden, S. M., G. D. Gwanmesia, J. D. Fitz Gerald, I. Jackson, R. C. Liebermann, Spinel elasticity and seismic structure of the transition zone of the mantle. Nature, 354, 143-145, 1991.
79. Ringwood AE., Role of the transition zone and 660 km discontinuity in mantle dynamics, Phys. Earth Planet. Inter, 86, 5-24, 1994.
80. 20, Earth Planet. Sci. Lett., 2, 130-133, 1967.
81. Rubie, D. C. and C. R. Ross II, Kinetics of olivine-spinel transformation in subducting lithosphere: experimental constraints and implications on deep slab processes, Phys. Earth Planet. Inter. 86, 223-241, 1994.
82. 3OH and aluminum oxide hydroxide δ-AlOOH at high pressure and temperature, J. Phys. Chem. Solids, 65, 1547-1554, 2004.
83. Schmidt, M. W., Lawsonite: Upper pressure stability and formation of higher density hydrous phases, Am. Mineral, 80, 1286-1292, 1995.
84. Schmidt, M. W. and S. Poli, Experimental base water budgets for dehydrating slabs and consequences for arc magma generation. Earth Planet. Sci. Lett., 163, 361-379, 1998.
85. 3(OH), a high-pressure hydrous phase, Am. Miner., 83, 881-888, 1998.
86. Shieh, S. R., H. K. Mao, and J. C. Ming, Decomposition of phase D in the lower mantle and the fate of dense hydrous silicates in subducting slabs, Earth Planet. Sci. Lett., 159, 13-23, 1998.
87. 3 perovskite at 8 GPa and 800 K and lower mantle composition, Science 281, 677-679, 1998.
88. Smyth, R., C. M. Holl, D. J. Frost, and S. D. Jacobsen, High pressure crystal chemistry of hydrous ringwoodite and water in the earth's interior, Phys. Earth Planet. Inter., 143-144, 271-278, 2004.
89. 2 at high pressure, in Core-mantle boundary region. Edited by M. Gurnis, M. E. Wysession, E. Knittle, and B. A. Buffet, Geodynamics Series, 28, AGU, pp83-96, 1998.
90. Suzuki, I., Thermal expansion of periclase and olivine, and their anharmonic properties. J. Phys. Earth, 23, 145-159, 1975.
91. Suzuki, I. and O. L. Anderson, Elasticity and thermal expansion of a natural garnet up to 1000 K, J. Phys. Earth, 31, 125-138, 1983.
92. Suzuki, A., E. Ohtani, and T. Kamada, A new hydrous phase 8-AlOOH synthesized at 20.9 GPa and 1000°C, Phys. Chem. Miner. 27, 689-693, 2000.
93. Ulmer, P and V. Trommsdorff, Serpentine stability to mantle depths and subduction related magmatism, Science, 268, 858-861, 1995.
94. Vanpeteghem, C. B., E. Ohtani, and T. Kondo, Equation of state of the hydrous phase δ-AlOOH at room temperature up to 22.5 GPa, Geophys. Res. Lett, 29, 7,10.1029, 2002.
95. 3 perovskite and implications for the lower mantle. Geophys. Res. Lett. 21, 895-898, 1994.
96. 3 perovskite. J. Geophys. Res. 101, 661-672, 1996.
97. 4. J. Geophys. Res. 89, 7852-7860, 1984.
98. Williams, Q, and R. J. Hemley, Hydrogen in the deep earth, Ann. Rev. Earth Planet. Sci., 29, 365-418, 2001.
99. Williams, Q. and E. J. Garnero, Seismic evidence for partial melting at the base of the lower mantle, Science, 273, 1528-1530, 1996.
100. 2: a fully hydrated analogue of topaz, Am. Mineral, 78, 285-297, 1997.
101. Yeganeh-Haeri, A., Synthesis and re-investigation of elastic properties of single-crystal magnesium silicate perovskite. Phys. Earth Planet. Inter. 87, 111-121, 1994.
102. Zhao, D., Seismological structure of subduction zones and its implications for arc magmatism and dynamics, Phys. Earth Planet. Inter, 127, 197-214, 2001.
103. Zhao, D., Global tomographic images of mantle plumes and subducting slabs: Insight into deep Earth dynamics, Phys. Earth Planet. Inter, 146, 3-34, 2004.
104. Zhao, D., Y. Xu, D. Wiens, L. Dorman, J. Hildebrand, S. Webb, Depth extent of the Lau back-arc spreading center and its relation to subduction processes, Science, 278, 254-257, 1997.