메뉴 건너뛰기




Volumn 111, Issue 6, 2006, Pages

Stability of anhydrous phase B: Experimental studies and implications for phase relations in subducting slab and the X discontinuity in the mantle

Author keywords

[No Author keywords available]

Indexed keywords

DISSOLUTION; EXPERIMENTAL MINERALOGY; FORSTERITE; MANTLE DISCONTINUITY; MELTING; P-T CONDITIONS; PERICLASE; PHASE EQUILIBRIUM; RINGWOODITE; SLAB; STISHOVITE; SUBDUCTION ZONE; WADSLEYITE;

EID: 33750498450     PISSN: 21699313     EISSN: 21699356     Source Type: Journal    
DOI: 10.1029/2005JB003910     Document Type: Article
Times cited : (37)

References (35)
  • 1
    • 0034649518 scopus 로고    scopus 로고
    • Possible presence of high-pressure ice in cold subducting slabs
    • Bina, C. R., and A. Navrotsky (2000), Possible presence of high-pressure ice in cold subducting slabs, Nature, 408, 844-847.
    • (2000) Nature , vol.408 , pp. 844-847
    • Bina, C.R.1    Navrotsky, A.2
  • 2
    • 0029519598 scopus 로고
    • Experimental and theoretical studies of the stabilities of talc, antigorite and phase A at high pressure with applications to subduction processes
    • Bose, K., and J. Ganguly (1995), Experimental and theoretical studies of the stabilities of talc, antigorite and phase A at high pressure with applications to subduction processes, Earth Planet. Sci. Lett., 136, 109-121.
    • (1995) Earth Planet. Sci. Lett. , vol.136 , pp. 109-121
    • Bose, K.1    Ganguly, J.2
  • 3
    • 0031466193 scopus 로고    scopus 로고
    • Rates and mechanisms of Fe-Mg interdiffusion in olivine at 980°-1300°C
    • Chakraborty, S. (1997), Rates and mechanisms of Fe-Mg interdiffusion in olivine at 980°-1300°C, J. Geophys. Res., 102, 12,317-12,331.
    • (1997) J. Geophys. Res. , vol.102
    • Chakraborty, S.1
  • 6
    • 0024879754 scopus 로고
    • o) of silicate minerals at 298 K from the sum of polyhedral contributions
    • o) of silicate minerals at 298 K from the sum of polyhedral contributions, Am. Mineral., 74, 1023-1031.
    • (1989) Am. Mineral. , vol.74 , pp. 1023-1031
    • Chermak, J.A.1    Rimstidt, J.D.2
  • 7
    • 0026452513 scopus 로고
    • Physical model of source region of subduction zone volcanics
    • Davies, J. H., and D. J. Stevenson (1992), Physical model of source region of subduction zone volcanics, J. Geophys. Res., 97, 2037-2070.
    • (1992) J. Geophys. Res. , vol.97 , pp. 2037-2070
    • Davies, J.H.1    Stevenson, D.J.2
  • 8
    • 22944488903 scopus 로고    scopus 로고
    • Pressure and temperature-dependence of water solubility in Fe-free wadsleyite
    • Demouchy, S., E. Deloule, D. J. Frost, and H. Keppler (2005), Pressure and temperature-dependence of water solubility in Fe-free wadsleyite, Am. Mineral., 90, 1084-1091.
    • (2005) Am. Mineral. , vol.90 , pp. 1084-1091
    • Demouchy, S.1    Deloule, E.2    Frost, D.J.3    Keppler, H.4
  • 11
    • 0037293243 scopus 로고    scopus 로고
    • 4 phases of the transition zone
    • 4 phases of the transition zone, Am. Mineral., 88, 387-397.
    • (2003) Am. Mineral. , vol.88 , pp. 387-397
    • Frost, D.J.1
  • 13
    • 4644324417 scopus 로고    scopus 로고
    • Diffusion kinetics in minerals: Principles and applications to tectono-metamorphic processes
    • in Eötvös Univ. Press, Budapest
    • Ganguly, J. (2002), Diffusion kinetics in minerals: Principles and applications to tectono-metamorphic processes, in Energy Modelling in Minerals, EMU Notes Mineral., vol. 4, pp. 271-309, Eötvös Univ. Press, Budapest.
    • (2002) Energy Modelling in Minerals, EMU Notes Mineral. , vol.4 , pp. 271-309
    • Ganguly, J.1
  • 15
    • 0042885665 scopus 로고    scopus 로고
    • Receiver functions in the western United States, with implications for upper mantle structure and dynamics
    • doi:10.1029/2001JB001194
    • Gilbert, H. J., A. F. Sheehan, K. G. Dueker, and P. Molnar (2003), Receiver functions in the western United States, with implications for upper mantle structure and dynamics, J. Geophys. Res., 108(B5), 2229, doi:10.1029/2001JB001194.
    • (2003) J. Geophys. Res. , vol.108 , Issue.B5 , pp. 2229
    • Gilbert, H.J.1    Sheehan, A.F.2    Dueker, K.G.3    Molnar, P.4
  • 16
    • 0041774753 scopus 로고
    • Melting experiments on chondrite at high pressures: Stability of anhydrous B
    • Herzberg, C. H., and T. Gasparik (1989), Melting experiments on chondrite at high pressures: Stability of anhydrous B, Eos Trans. AGU, 70(16), 484.
    • (1989) Eos Trans. AGU , vol.70 , Issue.16 , pp. 484
    • Herzberg, C.H.1    Gasparik, T.2
  • 17
    • 0029772078 scopus 로고    scopus 로고
    • Melting experiments on anhydrous peridotie KLB-1: Compositions of magma in the upper mantle and transition zone
    • Herzberg, C. H., and J. Zhang (1996), Melting experiments on anhydrous peridotie KLB-1: Compositions of magma in the upper mantle and transition zone, J. Geophys. Res., 101, 8271-8295.
    • (1996) J. Geophys. Res. , vol.101 , pp. 8271-8295
    • Herzberg, C.H.1    Zhang, J.2
  • 19
    • 0001326291 scopus 로고
    • Dependence of entropy on volume for silicate and oxide minerals: A review and predictive model
    • Holland, T. J. B. (1989), Dependence of entropy on volume for silicate and oxide minerals: A review and predictive model, Am. Mineral., 74, 5-13.
    • (1989) Am. Mineral. , vol.74 , pp. 5-13
    • Holland, T.J.B.1
  • 20
    • 17644405811 scopus 로고    scopus 로고
    • Water in the transition zone from electrical conductivity of wadseleyite and ringwoodite
    • Huang, X., Y. Xu, and S.I. Karato (2005), Water in the transition zone from electrical conductivity of wadseleyite and ringwoodite, Nature, 434, 746-749.
    • (2005) Nature , vol.434 , pp. 746-749
    • Huang, X.1    Xu, Y.2    Karato, S.I.3
  • 21
    • 0022265342 scopus 로고
    • Stability of phase B, a hydrous magnesium silicate, to 2300°C at 23 GPA
    • Kato, T., and M. Kumazawa (1985), Stability of phase B, a hydrous magnesium silicate, to 2300°C at 23 GPA, Geophys. Res. Lett., 12, 534-535.
    • (1985) Geophys. Res. Lett. , vol.12 , pp. 534-535
    • Kato, T.1    Kumazawa, M.2
  • 22
    • 33750529239 scopus 로고    scopus 로고
    • Introduction to minerals under extreme conditions
    • in edited by R. Miletich, Eötvös Univ. Press, Budapest, in press
    • Keppler, H., and D. J. Frost (2005), Introduction to minerals under extreme conditions, in Mineral Behaviour at Extreme Conditions, EMU Notes Mineral., vol. 7, edited by R. Miletich, Eötvös Univ. Press, Budapest, in press.
    • (2005) Mineral Behaviour at Extreme Conditions, EMU Notes Mineral. , vol.7
    • Keppler, H.1    Frost, D.J.2
  • 24
  • 25
    • 0026312660 scopus 로고
    • Mantle layering from ScS reverberations: 3. The upper mantle
    • Revenaugh, J., and T. H. Jordan (1991), Mantle layering from ScS reverberations: 3. The upper mantle, J. Geophys. Res., 96, 19,781-19,810.
    • (1991) J. Geophys. Res. , vol.96
    • Revenaugh, J.1    Jordan, T.H.2
  • 26
    • 33750506179 scopus 로고    scopus 로고
    • The seismic X discontinuity: Observations and modeling
    • Fall Meet. Suppl., Abstract S21E-05
    • Revenaugh, J., and Q. Williams (2000), The seismic X discontinuity: Observations and modeling, Eos Trans. AGU, 81(48), Fall Meet. Suppl., Abstract S21E-05.
    • (2000) Eos Trans. AGU , vol.81 , Issue.48
    • Revenaugh, J.1    Williams, Q.2
  • 30
    • 0023476862 scopus 로고
    • 4: A potential host for water in the mantle?
    • 4: A potential host for water in the mantle?, Am. Mineral, 72, 1051-1055.
    • (1987) Am. Mineral , vol.72 , pp. 1051-1055
    • Smyth, J.R.1
  • 32
    • 0027088335 scopus 로고
    • A model for the global variation of oceanic depth and heat flow with lithospheric age
    • Stein, C. A., and S. A. Stein (1992), A model for the global variation of oceanic depth and heat flow with lithospheric age, Nature, 359, 123-129.
    • (1992) Nature , vol.359 , pp. 123-129
    • Stein, C.A.1    Stein, S.A.2
  • 33
    • 0001601842 scopus 로고    scopus 로고
    • The X-discontinuity: A signature of deep fluid flow and free silica in the sub-continental mantle
    • Fall Meet. Suppl., Abstract S21E-07
    • Williams, Q., and J. S. Revenaugh (2000), The X-discontinuity: A signature of deep fluid flow and free silica in the sub-continental mantle, Eos Trans. AGU, 81(48), Fall Meet. Suppl., Abstract S21E-07.
    • (2000) Eos Trans. AGU , vol.81 , Issue.48
    • Williams, Q.1    Revenaugh, J.S.2
  • 34
    • 0028862657 scopus 로고
    • 2O on the 410-kilometer seismic discontinuity
    • 2O on the 410-kilometer seismic discontinuity, Science, 268, 74-76.
    • (1995) Science , vol.268 , pp. 74-76
    • Wood, B.J.1
  • 35
    • 0032522161 scopus 로고    scopus 로고
    • The orthorhombic to high-P monoclinic phase transition in Mg-Fe pyroxene: Can it produce a seismic discontinuity?
    • Woodland, A. B. (1998), The orthorhombic to high-P monoclinic phase transition in Mg-Fe pyroxene: Can it produce a seismic discontinuity?, Geophys. Res. Lett., 25, 1241-1244.
    • (1998) Geophys. Res. Lett. , vol.25 , pp. 1241-1244
    • Woodland, A.B.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.