AustralieFrV1, PascalFrancis, Curation, bibRecord, 003A49

Thermal properties of Australian sedimentary opals and Czech moldavites

Identifieur interne : 003A49 ( PascalFrancis/Curation ); précédent : 003A48; suivant : 003A50

Thermal properties of Australian sedimentary opals and Czech moldavites

Auteurs : P. S. Thomas [Australie] ; J. Sestak [République tchèque] ; K. Heide [Allemagne] ; E. Fueglein [Allemagne] ; P. Simon [Slovaquie]

Source :

Journal of thermal analysis and calorimetry [ 1388-6150 ] ; 2010.

RBID : Pascal:10-0338238

Descripteurs français

Pascal (Inist)
- Propriété thermique, Opale, Etat amorphe, Silice, Calorimétrie différentielle balayage, Thermogravimétrie, Méthode couplée, Analyse thermomécanique, Moldavite, Australie, République tchèque, Analyse thermique, Analyse gaz, Dégagement gazeux, Analyse gaz dégagé.
Wicri :
- geographic : Australie, République tchèque.

English descriptors

KwdEn :
- Amorphous state, Australia, Coupled method, Czech Republic, Differential scanning calorimetry, Evolved gas analysis, Gas analysis, Gas release, Moldavite, Opal, Silica, Thermal analysis, Thermal properties, Thermogravimetry, Thermomechanical analysis.

Abstract

The thermal properties are presented for a precious opal sourced from Coober Pedy, South Australia and a moldavite from Bohemia, Czech Republic whose origins differ significantly as opal is derived from the slow isothermal diagenesis of silica, while the tektites are specimens of vitreous silica formed from the terrestrial impact of asteroids. The differences between the two glassy silicates are presented through measurement of the TG-DSC, TMA and high-vacuum-hot-extraction DEGAS analysis.

A01	`01`	`1`		`@0 1388-6150`
A03		`1`		`@0 J. therm. anal. calorim.`
A05				`@2 99`
A06				`@2 3`
A08	`01`	`1`	`ENG`	`@1 Thermal properties of Australian sedimentary opals and Czech moldavites`
A09	`01`	`1`	`ENG`	`@1 The 9th Mediterranean conference on Colorimetry and Thermal Analysis: MEDICTA 2009, 15-18 June, 2009, Marseille, France: Selected papers`
A11	`01`	`1`		`@1 THOMAS (P. S.)`
A11	`02`	`1`		`@1 SESTAK (J.)`
A11	`03`	`1`		`@1 HEIDE (K.)`
A11	`04`	`1`		`@1 FUEGLEIN (E.)`
A11	`05`	`1`		`@1 SIMON (P.)`
A12	`01`	`1`		`@1 ROUQUEROL (Jean) @9 ed.`
A12	`02`	`1`		`@1 BEURROIES (Isabelle) @9 ed.`
A14	`01`			`@1 Department of Chemistry and Forensic Sciences, University of Technology Sydney, PO Box 123 @2 Sydney, NSW 2007 @3 AUS @Z 1 aut.`
A14	`02`			`@1 Solid-State Physics Section, Institute of Physics, Academy of Sciences, v.v.i., Cukrovarnická 10 @2 162 53 Praha @3 CZE @Z 2 aut.`
A14	`03`			`@1 Chemisch-Geowissenschaftliche Fakultat, Universitat Jena, Burgweg 11 @2 07749 Jena @3 DEU @Z 3 aut.`
A14	`04`			`@1 Netzsch-Gerätebau GmbH, Wittelsbacherstrasse 42 @2 95100 Selb @3 DEU @Z 4 aut.`
A14	`05`			`@1 Department of Physical Chemistry, Faculty of Chemical and Food Technology, Slovak University of Technology, Radlinského 9 @2 812 37 Bratislava @3 SVK @Z 5 aut.`
A15	`01`			`@1 Laboratoire Chimie Provence, Universités d'Aix-Marseille I, II, III et CNRS UMR6264, Site MADIREL, Centre de Saint Jérôme @2 13397 Marseille @3 FRA @Z 1 aut. @Z 2 aut.`
A20				`@1 861-867`
A21				`@1 2010`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 6367 @5 354000181909920210`
A44				`@0 0000 @1 © 2010 INIST-CNRS. All rights reserved.`
A45				`@0 30 ref.`
A47	`01`	`1`		`@0 10-0338238`
A60				`@1 P @2 C`
A61				`@0 A`
A64	`01`	`1`		`@0 Journal of thermal analysis and calorimetry`
A66	`01`			`@0 NLD`
C01	`01`		`ENG`	`@0 The thermal properties are presented for a precious opal sourced from Coober Pedy, South Australia and a moldavite from Bohemia, Czech Republic whose origins differ significantly as opal is derived from the slow isothermal diagenesis of silica, while the tektites are specimens of vitreous silica formed from the terrestrial impact of asteroids. The differences between the two glassy silicates are presented through measurement of the TG-DSC, TMA and high-vacuum-hot-extraction DEGAS analysis.`
C02	`01`	`X`		`@0 001C02B06`
C03	`01`	`X`	`FRE`	`@0 Propriété thermique @5 01`
C03	`01`	`X`	`ENG`	`@0 Thermal properties @5 01`
C03	`01`	`X`	`SPA`	`@0 Propiedad térmica @5 01`
C03	`02`	`X`	`FRE`	`@0 Opale @5 02`
C03	`02`	`X`	`ENG`	`@0 Opal @5 02`
C03	`02`	`X`	`SPA`	`@0 Opalo @5 02`
C03	`03`	`X`	`FRE`	`@0 Etat amorphe @5 03`
C03	`03`	`X`	`ENG`	`@0 Amorphous state @5 03`
C03	`03`	`X`	`SPA`	`@0 Estado amorfo @5 03`
C03	`04`	`X`	`FRE`	`@0 Silice @2 NK @2 FX @5 04`
C03	`04`	`X`	`ENG`	`@0 Silica @2 NK @2 FX @5 04`
C03	`04`	`X`	`SPA`	`@0 Sílice @2 NK @2 FX @5 04`
C03	`05`	`X`	`FRE`	`@0 Calorimétrie différentielle balayage @5 05`
C03	`05`	`X`	`ENG`	`@0 Differential scanning calorimetry @5 05`
C03	`05`	`X`	`SPA`	`@0 Análisis calorimétrico barrido exploración @5 05`
C03	`06`	`X`	`FRE`	`@0 Thermogravimétrie @5 06`
C03	`06`	`X`	`ENG`	`@0 Thermogravimetry @5 06`
C03	`06`	`X`	`SPA`	`@0 Termogravimetría @5 06`
C03	`07`	`X`	`FRE`	`@0 Méthode couplée @5 07`
C03	`07`	`X`	`ENG`	`@0 Coupled method @5 07`
C03	`07`	`X`	`SPA`	`@0 Método acoplado @5 07`
C03	`08`	`X`	`FRE`	`@0 Analyse thermomécanique @5 08`
C03	`08`	`X`	`ENG`	`@0 Thermomechanical analysis @5 08`
C03	`08`	`X`	`SPA`	`@0 Análisis termomecánico @5 08`
C03	`09`	`X`	`FRE`	`@0 Moldavite @5 09`
C03	`09`	`X`	`ENG`	`@0 Moldavite @5 09`
C03	`09`	`X`	`SPA`	`@0 Moldavita @5 09`
C03	`10`	`X`	`FRE`	`@0 Australie @2 NG @5 10`
C03	`10`	`X`	`ENG`	`@0 Australia @2 NG @5 10`
C03	`10`	`X`	`SPA`	`@0 Australia @2 NG @5 10`
C03	`11`	`X`	`FRE`	`@0 République tchèque @2 NG @5 11`
C03	`11`	`X`	`ENG`	`@0 Czech Republic @2 NG @5 11`
C03	`11`	`X`	`SPA`	`@0 República checa @2 NG @5 11`
C03	`12`	`X`	`FRE`	`@0 Analyse thermique @5 32`
C03	`12`	`X`	`ENG`	`@0 Thermal analysis @5 32`
C03	`12`	`X`	`SPA`	`@0 Análisis térmico @5 32`
C03	`13`	`X`	`FRE`	`@0 Analyse gaz @5 33`
C03	`13`	`X`	`ENG`	`@0 Gas analysis @5 33`
C03	`13`	`X`	`SPA`	`@0 Análisis gas @5 33`
C03	`14`	`X`	`FRE`	`@0 Dégagement gazeux @5 34`
C03	`14`	`X`	`ENG`	`@0 Gas release @5 34`
C03	`14`	`X`	`SPA`	`@0 Desprendimiento gaseoso @5 34`
C03	`15`	`X`	`FRE`	`@0 Analyse gaz dégagé @4 CD @5 96`
C03	`15`	`X`	`ENG`	`@0 Evolved gas analysis @4 CD @5 96`
C07	`01`	`X`	`FRE`	`@0 Océanie @2 NG`
C07	`01`	`X`	`ENG`	`@0 Oceania @2 NG`
C07	`01`	`X`	`SPA`	`@0 Oceania @2 NG`
C07	`02`	`X`	`FRE`	`@0 Europe @2 NG`
C07	`02`	`X`	`ENG`	`@0 Europe @2 NG`
C07	`02`	`X`	`SPA`	`@0 Europa @2 NG`
N21				`@1 214`

A30	`01`	`1`	`ENG`	`@1 Mediterranean Conference on Calorimetry and Thermal Analysis (MEDICTA 2009) @2 9 @3 Marseille FRA @4 2009-06-15`

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Le document en format XML

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<term>Thermogravimétrie</term>
<term>Méthode couplée</term>
<term>Analyse thermomécanique</term>
<term>Moldavite</term>
<term>Australie</term>
<term>République tchèque</term>
<term>Analyse thermique</term>
<term>Analyse gaz</term>
<term>Dégagement gazeux</term>
<term>Analyse gaz dégagé</term>
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<front><div type="abstract" xml:lang="en">The thermal properties are presented for a precious opal sourced from Coober Pedy, South Australia and a moldavite from Bohemia, Czech Republic whose origins differ significantly as opal is derived from the slow isothermal diagenesis of silica, while the tektites are specimens of vitreous silica formed from the terrestrial impact of asteroids. The differences between the two glassy silicates are presented through measurement of the TG-DSC, TMA and high-vacuum-hot-extraction DEGAS analysis.</div>
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<inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>1388-6150</s0>
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<fA08 i1="01" i2="1" l="ENG"><s1>Thermal properties of Australian sedimentary opals and Czech moldavites</s1>
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<fA09 i1="01" i2="1" l="ENG"><s1>The 9th Mediterranean conference on Colorimetry and Thermal Analysis: MEDICTA 2009, 15-18 June, 2009, Marseille, France: Selected papers</s1>
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<fA11 i1="01" i2="1"><s1>THOMAS (P. S.)</s1>
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<fA12 i1="01" i2="1"><s1>ROUQUEROL (Jean)</s1>
<s9>ed.</s9>
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<fA12 i1="02" i2="1"><s1>BEURROIES (Isabelle)</s1>
<s9>ed.</s9>
</fA12>
<fA14 i1="01"><s1>Department of Chemistry and Forensic Sciences, University of Technology Sydney, PO Box 123</s1>
<s2>Sydney, NSW 2007</s2>
<s3>AUS</s3>
<sZ>1 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Solid-State Physics Section, Institute of Physics, Academy of Sciences, v.v.i., Cukrovarnická 10</s1>
<s2>162 53 Praha</s2>
<s3>CZE</s3>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Chemisch-Geowissenschaftliche Fakultat, Universitat Jena, Burgweg 11</s1>
<s2>07749 Jena</s2>
<s3>DEU</s3>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>Netzsch-Gerätebau GmbH, Wittelsbacherstrasse 42</s1>
<s2>95100 Selb</s2>
<s3>DEU</s3>
<sZ>4 aut.</sZ>
</fA14>
<fA14 i1="05"><s1>Department of Physical Chemistry, Faculty of Chemical and Food Technology, Slovak University of Technology, Radlinského 9</s1>
<s2>812 37 Bratislava</s2>
<s3>SVK</s3>
<sZ>5 aut.</sZ>
</fA14>
<fA15 i1="01"><s1>Laboratoire Chimie Provence, Universités d'Aix-Marseille I, II, III et CNRS UMR6264, Site MADIREL, Centre de Saint Jérôme</s1>
<s2>13397 Marseille</s2>
<s3>FRA</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
</fA15>
<fA20><s1>861-867</s1>
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<s1>© 2010 INIST-CNRS. All rights reserved.</s1>
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<fA45><s0>30 ref.</s0>
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<fA60><s1>P</s1>
<s2>C</s2>
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<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Journal of thermal analysis and calorimetry</s0>
</fA64>
<fA66 i1="01"><s0>NLD</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>The thermal properties are presented for a precious opal sourced from Coober Pedy, South Australia and a moldavite from Bohemia, Czech Republic whose origins differ significantly as opal is derived from the slow isothermal diagenesis of silica, while the tektites are specimens of vitreous silica formed from the terrestrial impact of asteroids. The differences between the two glassy silicates are presented through measurement of the TG-DSC, TMA and high-vacuum-hot-extraction DEGAS analysis.</s0>
</fC01>
<fC02 i1="01" i2="X"><s0>001C02B06</s0>
</fC02>
<fC03 i1="01" i2="X" l="FRE"><s0>Propriété thermique</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="ENG"><s0>Thermal properties</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="SPA"><s0>Propiedad térmica</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE"><s0>Opale</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG"><s0>Opal</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA"><s0>Opalo</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Etat amorphe</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG"><s0>Amorphous state</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Estado amorfo</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE"><s0>Silice</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG"><s0>Silica</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA"><s0>Sílice</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Calorimétrie différentielle balayage</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Differential scanning calorimetry</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Análisis calorimétrico barrido exploración</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Thermogravimétrie</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Thermogravimetry</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Termogravimetría</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE"><s0>Méthode couplée</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG"><s0>Coupled method</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA"><s0>Método acoplado</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE"><s0>Analyse thermomécanique</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG"><s0>Thermomechanical analysis</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>Análisis termomecánico</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Moldavite</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Moldavite</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Moldavita</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE"><s0>Australie</s0>
<s2>NG</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG"><s0>Australia</s0>
<s2>NG</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA"><s0>Australia</s0>
<s2>NG</s2>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE"><s0>République tchèque</s0>
<s2>NG</s2>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG"><s0>Czech Republic</s0>
<s2>NG</s2>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA"><s0>República checa</s0>
<s2>NG</s2>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="X" l="FRE"><s0>Analyse thermique</s0>
<s5>32</s5>
</fC03>
<fC03 i1="12" i2="X" l="ENG"><s0>Thermal analysis</s0>
<s5>32</s5>
</fC03>
<fC03 i1="12" i2="X" l="SPA"><s0>Análisis térmico</s0>
<s5>32</s5>
</fC03>
<fC03 i1="13" i2="X" l="FRE"><s0>Analyse gaz</s0>
<s5>33</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG"><s0>Gas analysis</s0>
<s5>33</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA"><s0>Análisis gas</s0>
<s5>33</s5>
</fC03>
<fC03 i1="14" i2="X" l="FRE"><s0>Dégagement gazeux</s0>
<s5>34</s5>
</fC03>
<fC03 i1="14" i2="X" l="ENG"><s0>Gas release</s0>
<s5>34</s5>
</fC03>
<fC03 i1="14" i2="X" l="SPA"><s0>Desprendimiento gaseoso</s0>
<s5>34</s5>
</fC03>
<fC03 i1="15" i2="X" l="FRE"><s0>Analyse gaz dégagé</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fC03 i1="15" i2="X" l="ENG"><s0>Evolved gas analysis</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fC07 i1="01" i2="X" l="FRE"><s0>Océanie</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="X" l="ENG"><s0>Oceania</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="X" l="SPA"><s0>Oceania</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="X" l="FRE"><s0>Europe</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="X" l="ENG"><s0>Europe</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="X" l="SPA"><s0>Europa</s0>
<s2>NG</s2>
</fC07>
<fN21><s1>214</s1>
</fN21>
</pA>
<pR><fA30 i1="01" i2="1" l="ENG"><s1>Mediterranean Conference on Calorimetry and Thermal Analysis (MEDICTA 2009)</s1>
<s2>9</s2>
<s3>Marseille FRA</s3>
<s4>2009-06-15</s4>
</fA30>
</pR>
</standard>
</inist>
</record>

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	Serveur d'exploration sur les relations entre la France et l'Australie
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Serveur d'exploration sur les relations entre la France et l'Australie

Thermal properties of Australian sedimentary opals and Czech moldavites

Thermal properties of Australian sedimentary opals and Czech moldavites

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