Plastic deformation of minerals under extreme pressure using a multi-anvil apparatus

被引:48
作者
Cordier, P
Rubie, DC
机构
[1] Univ Sci & Tech Lille Flandres Artois, CNRS 8008, ESA, Lab Struct Proprietes Etat Solide, F-59655 Villeneuve Dascq, France
[2] Univ Bayreuth, Bayer Geoinst, D-95440 Bayreuth, Germany
来源
MATERIALS SCIENCE AND ENGINEERING A-STRUCTURAL MATERIALS PROPERTIES MICROSTRUCTURE AND PROCESSING | 2001年 / 309卷
关键词
plastic deformation; minerals; multi-anvil apparatus; high pressure;
D O I
10.1016/S0921-5093(00)01795-0
中图分类号
TB3 [工程材料学];
学科分类号
0805 ; 080502 ;
摘要
We describe recent progress in the achievement of high-pressure deformation experiments using the multi-anvil apparatus. This equipment allows experiments to be performed on samples that are several cubic millimeters in volume at pressures up to 26 GPa, corresponding to the uppermost lower mantle of the earth (700 km depth), and temperatures up to 2500 K. The high-pressure assemblies have been modified to induce plastic deformation under high-P, high-T conditions. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:38 / 43
页数:6
相关论文
共 23 条
[1]   Evaluation of the non-hydrostatic stress produced in a multi-anvil high pressure apparatus [J].
Ando, J ;
Irifune, T ;
Takeshita, T ;
Fujino, K .
PHYSICS AND CHEMISTRY OF MINERALS, 1997, 24 (02) :139-148
[2]   THE LARGE-VOLUME MULTI-ANVIL PRESS AS A HIGH P-T DEFORMATION APPARATUS [J].
BUSSOD, GY ;
KATSURA, T ;
RUBIE, DC .
PURE AND APPLIED GEOPHYSICS, 1993, 141 (2-4) :579-599
[3]   Strength and water weakening of mantle minerals, olivine, wadsleyite and ringwoodite (vol 25, pg 575, 1998) [J].
Chen, JH ;
Inoue, T ;
Weidner, DJ ;
Wu, YJ ;
Vaughan, MT .
GEOPHYSICAL RESEARCH LETTERS, 1998, 25 (07) :1103-1104
[4]   TEM investigation of dislocation microstructure of experimentally deformed silicate garnet [J].
Cordier, P ;
Raterron, P ;
Wang, Y .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1996, 97 (1-4) :121-131
[5]   ANALYTICAL ELECTRON-MICROSCOPY OF A SYNTHETIC PERIDOTITE EXPERIMENTALLY DEFORMED IN THE BETA-OLIVINE STABILITY FIELD [J].
DUPAS, C ;
DOUKHAN, N ;
DOUKHAN, JC ;
GREEN, HW ;
YOUNG, TE .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1994, 99 (B8) :15821-15832
[6]   Mechanisms of transformation and deformation in Mg1.8Fe0.2SiO4 olivine and wadsleyite under non-hydrostatic stress [J].
Dupas-Bruzek, C ;
Sharp, TG ;
Rubie, DC ;
Durham, WB .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1998, 108 (01) :33-48
[7]  
DURHAM WB, 1997, PROPERTIES EARTH PLA, P63
[8]   ANTICRACK-ASSOCIATED FAULTING AT VERY HIGH-PRESSURE IN NATURAL OLIVINE [J].
GREEN, HW ;
YOUNG, TE ;
WALKER, D ;
SCHOLZ, CH .
NATURE, 1990, 348 (6303) :720-722
[9]  
GREEN HW, 1989, EUR J MINERAL, V1, P213
[10]  
GRIGGS D, 1967, GEOPHYS J ROY ASTR S, V14, P19