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dc.contributor.authorBunge, H. J.
dc.contributor.authorKlein, H.
dc.contributor.authorWcislak, L.
dc.contributor.authorGarbe, U.
dc.contributor.authorWeiß, W.
dc.contributor.authorSchneider, J. R.
dc.date.accessioned2010-11-24T15:58:40Z
dc.date.available2010-11-24T15:58:40Z
dc.date.issued2003
dc.identifier.citationTextures and Microstructures; Vol. 35.2003, No. 3/4, p. 253-271
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0001-33F7-4
dc.description.abstractIn order to describe texture and microstructure of a polycrystalline material completely, crystal orientation g={?1F?2} must be known in all points x={x1?x2?x3} of the material. This can be achieved by locationresolved diffraction of high-energy, i.e. short-wave, X-rays from synchrotron sources. Highest resolution in the orientation- as well as the location-coordinates can be achieved by three variants of a detector sweeping technique in which an area detector is continuously moved during exposure. This technique results in two-dimensionally continuous images which are sections and projections of the six-dimensional orientation location space. Further evaluation of these images depends on whether individual grains are resolved in them or not. Because of the high penetration depth of high-energy synchrotron radiation in matter, this technique is also, and particularly, suitable for the investigation of the interior of big samples.
dc.format.extent18 S.
dc.format.mimetypeapplication/pdf
dc.language.isoeng
dc.relation.ispartofseriesTextures and Microstructures
dc.rights.urihttp://e-docs.geo-leo.de/rights
dc.subject.ddc548
dc.subject.gokVAE 120
dc.subject.gokVKA 200
dc.subject.gokVGA 410
dc.titleHigh-Resolution Imaging of Texture and Microstructure by the Moving Detector Method
dc.typearticle
dc.subject.gokverbalMethodik {Strukturgeologie}
dc.subject.gokverbalGefügekunde der Gesteine
dc.subject.gokverbalRöntgenanalyse {Mineralogie: Kristallographie}
dc.bibliographicCitation.volume35
dc.bibliographicCitation.issue3/4
dc.bibliographicCitation.firstPage253
dc.bibliographicCitation.lastPage271
dc.identifier.doi10.23689/fidgeo-833
dc.identifier.ppn571819583
dc.type.versionpublishedVersion
dc.bibliographicCitation.journalTextures and Microstructures
dc.relation.collectionGeologische Wissenschaften
dc.description.typeresearch


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