Dislocation generation, slip systems, and dynamic recrystallization in experimentally deformed plagioclase single crystals

dc.contributor.authorStunitz, H
dc.contributor.authorFitz Gerald, John
dc.contributor.authorTullis, J
dc.date.accessioned2015-12-13T22:28:43Z
dc.date.available2015-12-13T22:28:43Z
dc.date.issued2003
dc.date.updated2015-12-11T08:40:49Z
dc.description.abstractThree samples of gem quality plagioclase crystals of An60 were experimentally deformed at 900 °C, 1 GPa confining pressure and strain rates of 7.5-8.7×10-7s-1. The starting material is effectively dislocation-free so that all observed defects were intro
dc.identifier.issn0040-1951
dc.identifier.urihttp://hdl.handle.net/1885/74328
dc.publisherElsevier
dc.sourceTectonophysics
dc.subjectKeywords: deformation; fracture; microstructure; plagioclase; recrystallization; shear; twinning Dislocations; Dynamic recrystallization; Experimental deformation; Fracturing; Plagioclase deformation; Slip systems
dc.titleDislocation generation, slip systems, and dynamic recrystallization in experimentally deformed plagioclase single crystals
dc.typeJournal article
local.bibliographicCitation.lastpage233
local.bibliographicCitation.startpage215
local.contributor.affiliationStunitz, H, Universitat Basel
local.contributor.affiliationFitz Gerald, John, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationTullis, J, Brown University
local.contributor.authoremailu8001315@anu.edu.au
local.contributor.authoruidFitz Gerald, John, u8001315
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040312 - Structural Geology
local.identifier.absfor040306 - Mineralogy and Crystallography
local.identifier.ariespublicationMigratedxPub4064
local.identifier.citationvolume372
local.identifier.doi10.1016/S0040-1951(03)00241-5
local.identifier.scopusID2-s2.0-0141723695
local.identifier.uidSubmittedByMigrated
local.type.statusPublished Version

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