Viscosity of the albite melt to 7 GPa at 2000 K

被引:36
作者
Mori, S [1 ]
Ohtani, E [1 ]
Suzuki, A [1 ]
机构
[1] Tohoku Univ, Inst Mineral Petrol & Econ Geol, Sendai, Miyagi 9808578, Japan
关键词
viscosity; density; albite; silicate melts; high pressure;
D O I
10.1016/S0012-821X(99)00284-8
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 [地球物理学]; 070902 [地球化学];
摘要
Viscosity of melt at high pressure provides an important clue to understanding the dynamics of magmas in the Earth's deep interior. We measured viscosity of the albite melt to 7 GPa at 2000 K by the falling sphere method using a single crystalline diamond as a density marker. Viscosity of the melt decreases significantly from 5.28 +/- 1.78 Pa a at 3 GPa to 0.90 +/- 0.34 Pa s at 5 GPa and 0.99 +/- 0.27 Pa s at 6 GPa. We observed a further decrease in viscosity of the melt to 0.28 +/- 0.06 Pa s at 7 GPa. The change in viscosity with pressure may suggest existence of some structural change in the albite melt at high pressure. (C) 2000 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:87 / 92
页数:6
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