Rheology of synthetic polycrystalline halite in torsion

被引:15
|
作者
Marques, F. O. [1 ]
Burg, J. -P. [1 ]
Armann, M. [1 ]
Martinho, E. [1 ]
机构
[1] Swiss Fed Inst Technol, Dept Geosci, CH-8092 Zurich, Switzerland
关键词
Halite/rock salt; Rheology; Microstructure; Halite strength; Torsion experiments; ROCK-SALT; DYNAMIC RECRYSTALLIZATION; DEFORMATION; CREEP; BEHAVIOR; TESTS; WATER;
D O I
10.1016/j.tecto.2012.10.024
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
Motivated by the need for halite rheology, we investigated the stress/strain/strain rate behaviour of halite to high shear strains in torsion, using polymer jackets whose strength does not influence halite rheology. The experimental results show that: (1) halite strength decays exponentially with temperature increase, being very weak at 300 degrees C (ca. 2 Nm); (2) power-laws fit the stress/strain rate data, from which we determined the stress exponent n between ca. 13 (60 degrees C) and ca. 3 (200 degrees C), indicating that n decreases exponentially with temperature increase; (3) the activation energy Q decreases exponentially with temperature increase, from ca. 159 kJ/mol (38 kcal/mol) at 60 degrees C to ca. 59 kJ/mol (14 kcal/mol) at 200 degrees C; (4) Q depends linearly on n with a slope of ca. 10. The empirical constitutive equation (gamma) over dot = 12.1exp(9.6 + 7.1E-6exp(1/T1.9E-4))tau((25+93E6exp(-T/24 3))) describes the experimental results. Comparison of the present and previous experimental results shows that halite is much weaker in shear than in axial compression or extension. This difference likely results from the rotational component of simple shear. (C) 2012 Elsevier B.V. All rights reserved.
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页码:124 / 130
页数:7
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