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Strain softening and microstructural evolution of anorthite aggregates and quartz-anorthite layered composites deformed in torsion
Ji, SC; Jiang, ZT; Rybacki, E; Wirth, R; Prior, D; Xia, B; sji@polymtl.ca
2004
Source PublicationEARTH AND PLANETARY SCIENCE LETTERS
ISSN0012-821X
Volume222Issue:2Pages:377-390
AbstractTorsion experiments of anorthite (An) aggregates and layered composites with equal volume fractions of quartz (Qtz) and An were performed in a gas-medium apparatus at a confining pressure of 400 MPa, temperatures from 1373 to 1473 K, and twist rates from 1.0 x 10(-4) to 3.0 x 10(-4) rad/s. Dense specimens were fabricated from An glass and Qtz crystalline powder using hot isostatic pressing (HIP) techniques. Both An aggregates and Qtz-An layered composites show a continuous strain weakening from a peak stress at gamma=0.2-0.3 to gamma=3.2, and steady-state flow has not reached under the experimental conditions. The weakening is even more pronounced in the layered composites than the monolithic aggregates, suggesting channeling or localization of flow into the weak material between strong layers. The sheared An specimens developed pervasively C-S-C' structures which are similar to those observed in natural ductile shear zones. TEM and electron backscattering diffraction (EBSD) fabric analyses suggest that grain boundary migration recrystallization-accommodated dislocation creep with (010)[100] as the dominant slip system was operating in the An. The strain softening may be due to the development of crystallographic preferred orientation (CPO), the operation of dynamic recrystallization and the formation of extremely fine-grained recrystallized material in the narrow C' shear bands. (C) 2004 Elsevier B.V All rights reserved.
DepartmentEcole Polytech, Dept Genies Civil Geol & Mines, Montreal, PQ H3C 3A7, Canada; Univ Liverpool, Dept Earth Sci, Liverpool L69 3BX, Merseyside, England; Geoforschungszentrum Potsdam, D-14473 Potsdam, Germany; Chinese Acad Sci, Guangzhou Inst Geochem, Lab Marginal Sea Geol, Guangzhou, Peoples R China; Chinese Acad Sci, S China Sea Inst Oceanol, Guangzhou, Peoples R China
KeywordAnorthite Quartz-anorthite Composite Simple Shear Crystallographic Preferred Orientation Flow Strength
Subject AreaGeochemistry & Geophysics
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Indexed Bysci
Funding Project海洋地质
WOS IDWOS:000221993700004
Citation statistics
Cited Times:28[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.scsio.ac.cn/handle/344004/4802
Collection中科院边缘海地质重点实验室
Corresponding Authorsji@polymtl.ca
Recommended Citation
GB/T 7714
Ji, SC,Jiang, ZT,Rybacki, E,et al. Strain softening and microstructural evolution of anorthite aggregates and quartz-anorthite layered composites deformed in torsion[J]. EARTH AND PLANETARY SCIENCE LETTERS,2004,222(2):377-390.
APA Ji, SC.,Jiang, ZT.,Rybacki, E.,Wirth, R.,Prior, D.,...&sji@polymtl.ca.(2004).Strain softening and microstructural evolution of anorthite aggregates and quartz-anorthite layered composites deformed in torsion.EARTH AND PLANETARY SCIENCE LETTERS,222(2),377-390.
MLA Ji, SC,et al."Strain softening and microstructural evolution of anorthite aggregates and quartz-anorthite layered composites deformed in torsion".EARTH AND PLANETARY SCIENCE LETTERS 222.2(2004):377-390.
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