Thermal-mechanical effects of low-temperature plasticity (the Peierls mechanism) on the deformation of a viscoelastic shear zone

被引:145
作者
Kameyama, M
Yuen, DA
Karato, SI
机构
[1] Univ Minnesota, Minnesota Supercomp Inst, Minneapolis, MN 55415 USA
[2] Univ Minnesota, Dept Geol & Geophys, Minneapolis, MN 55415 USA
[3] Univ Tokyo, Ocean Res Inst, Tokyo 164, Japan
关键词
plasticity; rheology; thermomechanical properties; shear zones; subduction;
D O I
10.1016/S0012-821X(99)00040-0
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
We studied for the first time the effects of low-temperature plasticity on the formation of shear zones. A thermal-mechanical model has been developed for describing the shear deformation of Maxwell viscoelastic material with a rheology close to dry olivine. We employed a one-dimensional model with a half-width of L deforming under a constant velocity U at the boundary, and the spatially-averaged strain rate U/L was set to O(10(-14)) s(-1). In addition to diffusion and power-law creep, we included deformation by low-temperature plasticity, called the Peierls mechanism, which is significant at low temperatures and has a strong exponential dependence on the stress. When a sufficient magnitude of heat is generated by the rapid conversion from elastically-stored energy into viscous dissipation, thermal instability takes place and the defor mation localizes in a narrow region. By comparing the condition for thermal instability, we found that the low-temperature plasticity inhibits the development of thermal instability in shear zones in case of constant strain rate. The Peierls mechanism enhances deformation at a significantly lower stress compared to the rheology with solely diffusion creep and power-law creep. The enhanced deformation by low-temperature plasticity produces lower amount of dissipative heating, and thus stabilizes the shear zone. Comparing the stability between constant strain-rate and constant stress boundary conditions, we found that the Peierls mechanism exerts an opposite destabilizing effect in the case of constant stress. For dry olivine rheology and realistic magnitude of the strain rate, the effect of low-temperature plasticity is significant for temperatures between around 800 K and 1000 K. This finding suggests that the low-temperature plasticity may be crucial in determining the thermal-mechanical stability in the shallow portion of slabs. (C) 1999 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:159 / 172
页数:14
相关论文
共 37 条
[1]   Generation of plate tectonics from lithosphere-mantle flow and void-volatile self-lubrication [J].
Bercovici, D .
EARTH AND PLANETARY SCIENCE LETTERS, 1998, 154 (1-4) :139-151
[2]   A SIMPLE-MODEL OF PLATE GENERATION FROM MANTLE FLOW [J].
BERCOVICI, D .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1993, 114 (03) :635-650
[4]   AN EULERIAN TECHNIQUE FOR THERMOMECHANICAL MODELING OF LITHOSPHERIC EXTENSION [J].
CHRISTENSEN, UR .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1992, 97 (B2) :2015-2036
[5]  
Drozdov A.D., 1996, FINITE ELASTICITY VI
[6]   THE EFFECT OF TEMPERATURE AND IMPURITY CONTENT ON INDENTATION HARDNESS OF QUARTZ [J].
EVANS, B .
JOURNAL OF GEOPHYSICAL RESEARCH, 1984, 89 (NB6) :4213-4222
[7]   TEMPERATURE-VARIATION OF HARDNESS OF OLIVINE AND ITS IMPLICATION FOR POLYCRYSTALLINE YIELD STRESS [J].
EVANS, B ;
GOETZE, C .
JOURNAL OF GEOPHYSICAL RESEARCH, 1979, 84 (NB10) :5505-5524
[8]  
FLACK CA, 1990, GEOLOGY, V18, P528, DOI 10.1130/0091-7613(1990)018<0528:RFMFZA>2.3.CO
[9]  
2
[10]   THERMAL AND MECHANICAL EVOLUTION OF SHEAR ZONES [J].
FLEITOUT, L ;
FROIDEVAUX, C .
JOURNAL OF STRUCTURAL GEOLOGY, 1980, 2 (1-2) :159-164