UnivTrevesV1, PascalFrancis, Corpus, bibRecord, 001466

Determination and interpretation of preferred orientation with texture goniometry : An application of indicators to maximum entropy pole- to orientation-density inversion

Identifieur interne : 001466 ( PascalFrancis/Corpus ); précédent : 001465; suivant : 001467

Determination and interpretation of preferred orientation with texture goniometry : An application of indicators to maximum entropy pole- to orientation-density inversion

Auteurs : H. Schaeben ; H. Siemes

Source :

Mathematical geology [ 0882-8121 ] ; 1996.

RBID : Pascal:96-0201422

Descripteurs français

Pascal (Inist)
- Quartzite, Fabrique, Analyse texture, Orientation préférentielle, Goniométrie, Fonction densité, Méthode entropie maximum, Problème inverse, Tomographie, Analyse quantitative, Polycristal, Etude cas.

English descriptors

KwdEn :
- Case study, Density function, Goniometry, Inverse problem, Method of maximum entropy, Polycrystal, Preferred orientation, Quantitative analysis, Quartzites, Texture analysis, Tomography, fabric.

Abstract

The probability density function of orientations of crystals generally cannot be measured directly without destruction of the specimen. Therefore it is usual practice to sample pole density functions of several crystal forms in diffraction experiments with a texture goniometer. Determining a reasonable orientation density function from experimental pole density functions is then the crucial prerequisite of quantitative texture analysis. This mathematical problem may be addressed as a tomographic inversion problem specified by the crystal and statistical specimen symmetries and the properties of the diffraction experiment. Its solution with maximum entropy preferred orientation portion and maximum uniform portion is proposed because it yields the most conservative orientation density function with systematically reduced correlation effects, thus avoiding artificial texture "ghost" components caused by the specific properties of the diffraction experiment.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A02	`01`			`@0 MATGED`
A03		`1`		`@0 Math. geol.`
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A06				`@2 2`
A08	`01`	`1`	`ENG`	`@1 Determination and interpretation of preferred orientation with texture goniometry : An application of indicators to maximum entropy pole- to orientation-density inversion`
A09	`01`	`1`	`ENG`	`@1 Inverse theory in the earth sciences`
A11	`01`	`1`		`@1 SCHAEBEN (H.)`
A11	`02`	`1`		`@1 SIEMES (H.)`
A12	`01`	`1`		`@1 HERZFELD (Ute Christina) @9 ed.`
A14	`01`			`@1 Department of Mineralogy, University of Technology Aachen, Templergraben 55 @2 52056 Aachen @3 DEU @Z 1 aut. @Z 2 aut.`
A15	`01`			`@1 FB VI Quantitative Methoden in den Geowissenschaften, Universität Trier @2 54286 Trier @3 DEU @Z 1 aut.`
A15	`02`			`@1 Institute of Arctic and Alpine Research, University of Colorado Boulder @2 Boulder, Colorado 80309-0450 @3 USA @Z 1 aut.`
A20				`@1 169-201`
A21				`@1 1996`
A23	`01`			`@0 ENG`
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A60				`@1 P`
A61				`@0 A`
A64	`01`	`1`		`@0 Mathematical geology`
A66	`01`			`@0 USA`
C01	`01`		`ENG`	@0 The probability density function of orientations of crystals generally cannot be measured directly without destruction of the specimen. Therefore it is usual practice to sample pole density functions of several crystal forms in diffraction experiments with a texture goniometer. Determining a reasonable orientation density function from experimental pole density functions is then the crucial prerequisite of quantitative texture analysis. This mathematical problem may be addressed as a tomographic inversion problem specified by the crystal and statistical specimen symmetries and the properties of the diffraction experiment. Its solution with maximum entropy preferred orientation portion and maximum uniform portion is proposed because it yields the most conservative orientation density function with systematically reduced correlation effects, thus avoiding artificial texture "ghost" components caused by the specific properties of the diffraction experiment.
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C03	`01`	`X`	`ENG`	`@0 Quartzites @5 16`
C03	`01`	`X`	`SPA`	`@0 Cuarzita @5 16`
C03	`02`	`2`	`FRE`	`@0 Fabrique @5 17`
C03	`02`	`2`	`ENG`	`@0 fabric @5 17`
C03	`02`	`2`	`SPA`	`@0 Fábrica @5 17`
C03	`03`	`X`	`FRE`	`@0 Analyse texture @5 26`
C03	`03`	`X`	`ENG`	`@0 Texture analysis @5 26`
C03	`03`	`X`	`SPA`	`@0 Análisis textura @5 26`
C03	`04`	`X`	`FRE`	`@0 Orientation préférentielle @5 27`
C03	`04`	`X`	`ENG`	`@0 Preferred orientation @5 27`
C03	`04`	`X`	`GER`	`@0 Bevorzugte Orientierung @5 27`
C03	`04`	`X`	`SPA`	`@0 Orientación preferencial @5 27`
C03	`05`	`X`	`FRE`	`@0 Goniométrie @5 28`
C03	`05`	`X`	`ENG`	`@0 Goniometry @5 28`
C03	`05`	`X`	`SPA`	`@0 Goniometría @5 28`
C03	`06`	`X`	`FRE`	`@0 Fonction densité @5 29`
C03	`06`	`X`	`ENG`	`@0 Density function @5 29`
C03	`06`	`X`	`SPA`	`@0 Función densidad @5 29`
C03	`07`	`X`	`FRE`	`@0 Méthode entropie maximum @5 30`
C03	`07`	`X`	`ENG`	`@0 Method of maximum entropy @5 30`
C03	`07`	`X`	`SPA`	`@0 Método entropía máxima @5 30`
C03	`08`	`X`	`FRE`	`@0 Problème inverse @5 31`
C03	`08`	`X`	`ENG`	`@0 Inverse problem @5 31`
C03	`08`	`X`	`SPA`	`@0 Problema inverso @5 31`
C03	`09`	`X`	`FRE`	`@0 Tomographie @5 32`
C03	`09`	`X`	`ENG`	`@0 Tomography @5 32`
C03	`09`	`X`	`GER`	`@0 Tomographie @5 32`
C03	`09`	`X`	`SPA`	`@0 Tomografía @5 32`
C03	`10`	`X`	`FRE`	`@0 Analyse quantitative @5 33`
C03	`10`	`X`	`ENG`	`@0 Quantitative analysis @5 33`
C03	`10`	`X`	`GER`	`@0 Quantitative Analyse @5 33`
C03	`10`	`X`	`SPA`	`@0 Análisis cuantitativo @5 33`
C03	`11`	`X`	`FRE`	`@0 Polycristal @5 34`
C03	`11`	`X`	`ENG`	`@0 Polycrystal @5 34`
C03	`11`	`X`	`GER`	`@0 Polykristall @5 34`
C03	`11`	`X`	`SPA`	`@0 Policristal @5 34`
C03	`12`	`X`	`FRE`	`@0 Etude cas @5 35`
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C03	`12`	`X`	`SPA`	`@0 Estudio caso @5 35`
N21				`@1 134`

Format Inist (serveur)

NO :	PASCAL 96-0201422 INIST
ET :	Determination and interpretation of preferred orientation with texture goniometry : An application of indicators to maximum entropy pole- to orientation-density inversion
AU :	SCHAEBEN (H.); SIEMES (H.); HERZFELD (Ute Christina)
AF :	Department of Mineralogy, University of Technology Aachen, Templergraben 55/52056 Aachen/Allemagne (1 aut., 2 aut.); FB VI Quantitative Methoden in den Geowissenschaften, Universität Trier/54286 Trier/Allemagne (1 aut.); Institute of Arctic and Alpine Research, University of Colorado Boulder/Boulder, Colorado 80309-0450/Etats-Unis (1 aut.)
DT :	Publication en série; Niveau analytique
SO :	Mathematical geology; ISSN 0882-8121; Coden MATGED; Etats-Unis; Da. 1996; Vol. 28; No. 2; Pp. 169-201; Bibl. 3 p.1/2
LA :	Anglais
EA :	The probability density function of orientations of crystals generally cannot be measured directly without destruction of the specimen. Therefore it is usual practice to sample pole density functions of several crystal forms in diffraction experiments with a texture goniometer. Determining a reasonable orientation density function from experimental pole density functions is then the crucial prerequisite of quantitative texture analysis. This mathematical problem may be addressed as a tomographic inversion problem specified by the crystal and statistical specimen symmetries and the properties of the diffraction experiment. Its solution with maximum entropy preferred orientation portion and maximum uniform portion is proposed because it yields the most conservative orientation density function with systematically reduced correlation effects, thus avoiding artificial texture "ghost" components caused by the specific properties of the diffraction experiment.
CC :	001E01G04; 223A04
FD :	Quartzite; Fabrique; Analyse texture; Orientation préférentielle; Goniométrie; Fonction densité; Méthode entropie maximum; Problème inverse; Tomographie; Analyse quantitative; Polycristal; Etude cas
ED :	Quartzites; fabric; Texture analysis; Preferred orientation; Goniometry; Density function; Method of maximum entropy; Inverse problem; Tomography; Quantitative analysis; Polycrystal; Case study
GD :	Bevorzugte Orientierung; Tomographie; Quantitative Analyse; Polykristall
SD :	Cuarzita; Fábrica; Análisis textura; Orientación preferencial; Goniometría; Función densidad; Método entropía máxima; Problema inverso; Tomografía; Análisis cuantitativo; Policristal; Estudio caso
LO :	INIST-14907.354000053329610030
ID :	96-0201422

Links to Exploration step

Pascal:96-0201422

Le document en format XML

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<server><NO>PASCAL 96-0201422 INIST</NO>
<ET>Determination and interpretation of preferred orientation with texture goniometry : An application of indicators to maximum entropy pole- to orientation-density inversion</ET>
<AU>SCHAEBEN (H.); SIEMES (H.); HERZFELD (Ute Christina)</AU>
<AF>Department of Mineralogy, University of Technology Aachen, Templergraben 55/52056 Aachen/Allemagne (1 aut., 2 aut.); FB VI Quantitative Methoden in den Geowissenschaften, Universität Trier/54286 Trier/Allemagne (1 aut.); Institute of Arctic and Alpine Research, University of Colorado Boulder/Boulder, Colorado 80309-0450/Etats-Unis (1 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Mathematical geology; ISSN 0882-8121; Coden MATGED; Etats-Unis; Da. 1996; Vol. 28; No. 2; Pp. 169-201; Bibl. 3 p.1/2</SO>
<LA>Anglais</LA>
<EA>The probability density function of orientations of crystals generally cannot be measured directly without destruction of the specimen. Therefore it is usual practice to sample pole density functions of several crystal forms in diffraction experiments with a texture goniometer. Determining a reasonable orientation density function from experimental pole density functions is then the crucial prerequisite of quantitative texture analysis. This mathematical problem may be addressed as a tomographic inversion problem specified by the crystal and statistical specimen symmetries and the properties of the diffraction experiment. Its solution with maximum entropy preferred orientation portion and maximum uniform portion is proposed because it yields the most conservative orientation density function with systematically reduced correlation effects, thus avoiding artificial texture "ghost" components caused by the specific properties of the diffraction experiment.</EA>
<CC>001E01G04; 223A04</CC>
<FD>Quartzite; Fabrique; Analyse texture; Orientation préférentielle; Goniométrie; Fonction densité; Méthode entropie maximum; Problème inverse; Tomographie; Analyse quantitative; Polycristal; Etude cas</FD>
<ED>Quartzites; fabric; Texture analysis; Preferred orientation; Goniometry; Density function; Method of maximum entropy; Inverse problem; Tomography; Quantitative analysis; Polycrystal; Case study</ED>
<GD>Bevorzugte Orientierung; Tomographie; Quantitative Analyse; Polykristall</GD>
<SD>Cuarzita; Fábrica; Análisis textura; Orientación preferencial; Goniometría; Función densidad; Método entropía máxima; Problema inverso; Tomografía; Análisis cuantitativo; Policristal; Estudio caso</SD>
<LO>INIST-14907.354000053329610030</LO>
<ID>96-0201422</ID>
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Determination and interpretation of preferred orientation with texture goniometry : An application of indicators to maximum entropy pole- to orientation-density inversion

Determination and interpretation of preferred orientation with texture goniometry : An application of indicators to maximum entropy pole- to orientation-density inversion

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