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Effect of hydration on the single-crystal elasticity of Fe-bearing wadsleyite to 12 GPa
被引:49
|作者:
Mao, Zhu
[1
]
Jacobsen, Steven D.
[2
]
Frost, Daniel J.
[3
]
McCammon, Catherine A.
[3
]
Hauri, Erik H.
[4
]
Duffy, Thomas S.
[1
]
机构:
[1] Princeton Univ, Dept Geosci, Princeton, NJ 08544 USA
[2] Northwestern Univ, Dept Earth & Planetary Sci, Evanston, IL 60208 USA
[3] Univ Bayreuth, Bayer Geoinst, D-95440 Bayreuth, Germany
[4] Carnegie Inst Washington, Dept Terr Magnetism, Washington, DC 20015 USA
基金:
美国国家科学基金会;
关键词:
Fe-bearing hydrous wadsleyite;
elasticity;
Brillouin scattering;
transition zone;
high pressure;
KM SEISMIC DISCONTINUITY;
SAN CARLOS OLIVINE;
X-RAY-DIFFRACTION;
HYDROUS WADSLEYITE;
SOUND VELOCITIES;
UPPER-MANTLE;
EARTHS MANTLE;
BRILLOUIN-SCATTERING;
TRANSITION ZONE;
OXYGEN FUGACITY;
D O I:
10.2138/am.2011.3807
中图分类号:
P3 [地球物理学];
P59 [地球化学];
学科分类号:
0708 ;
070902 ;
摘要:
The single-crystal elastic properties of Fe-bearing wadsleyite with 1.93 wt% H(2)O (Mg(1.634)Fe(0.202)H(0.305)SiO(4)) have been determined by Brillouin scattering. At ambient conditions, the aggregate bulk and shear moduli (K(S0), G(0)) of this wadsleyite are 156.2(5) and 98.0(3) GPa, respectively. Compared to the corresponding anhydrous wadsleyite, 1.93 wt% H(2)O lowers K(S0) and G(0) by 8.1% and 9.3%, respectively. High-pressure measurements up to 12 GPa show that the pressure derivative of the bulk modulus, K'(S0)= 4.8(1), is similar to that of the anhydrous Fe-wadsleyite with reported values of 4.6-4.74, but the addition of H(2)O increases the pressure derivative of the shear modulus, G'(0) from 1.5(1) to 1.9(1). This contrasts with the G'(0) of Fe-free wadsleyite, which is the same within uncertainty for the hydrous and anhydrous phases. As a result, both the compressional- and shear-wave velocities (v(P), v(S)) of hydrous Fe-bearing wadsleyite are about 200(+/- 24) m/s slower than anhydrous Fe-bearing wadsleyite at transition zone pressures.
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页码:1606 / 1612
页数:7
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