In situ measurements of sound velocities and densities across the orthopyroxene → high-pressure clinopyroxene transition in MgSiO3 at high pressure

被引:116
|
作者
Kung, J [1 ]
Li, BS
Uchida, T
Wang, YB
Neuville, D
Liebermann, RC
机构
[1] SUNY Stony Brook, Inst Mineral Phys, Stony Brook, NY 11794 USA
[2] SUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USA
[3] Univ Chicago, Argonne Natl Lab, GSECARS, Ctr Adv Radiat Sources, Chicago, IL 60439 USA
[4] Inst Phys Globe, Lab Phys Geomat, F-75252 Paris, France
基金
美国国家科学基金会;
关键词
pyroxene; elasticity; high pressure; elastic softening; unquenchable; phase transformation;
D O I
10.1016/j.pepi.2004.05.008
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
Using acoustic measurement interfaced with a large volume multi-anvil apparatus in conjunction with in situ X-radiation techniques, we are able to measure the density and elastic wave velocities (V-P and V-S) for both ortho- and high-pressure clino-MgSiO3 polymorphs in the same experimental run. The elastic bulk and shear moduli of the unquenchable high-pressure clinoenstatite phase were measured within its stability field for the first time. The measured density contrast associated with the phase transition OEN --> HP-CEN is 2.6-2.9% in the pressure of 7-9 GPa, and the corresponding velocity jumps are 3-4% for P waves and 5-6% for S waves. The elastic moduli of the HP-CEN phase are K-S = 156.7(8) GPa, G = 98.5(4) GPa and their pressure derivatives are K'(S) = 5.5 (3) and G' = 1.5(1) at a pressure of 6.5 GPa, room temperature. In addition, we observed anomalous elastic behavior in orthoenstatite at pressure above 9 GPa at room temperature. Both elastic wave velocities exhibited softening between 9 and 13-14 GPa, which we suggest is associated with a transition to a metastable phase intermediate between OEN and HP-CEN. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:27 / 44
页数:18
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