Modelling the giant, Zn-Pb-Ag Century deposit, Queensland, Australia
Identifieur interne : 002991 ( PascalFrancis/Checkpoint ); précédent : 002990; suivant : 002992Modelling the giant, Zn-Pb-Ag Century deposit, Queensland, Australia
Auteurs : L. Feltrin [Australie] ; J. G. Mclellan [Australie] ; N. H. S. Oliver [Australie]Source :
- Computers & geosciences [ 0098-3004 ] ; 2009.
Descripteurs français
- Pascal (Inist)
- Modèle numérique, Méthode différence finie, Siltstone, Ecoulement, Ordinateur, Minéralisation, Genèse, Elément métallique, Zonation, Faille, Shale, Problème inverse, Zone faillée, Métal base, Diagenèse, Traitement donnée, Modèle 3 dimensions, Zinc, Plomb, Argent, Remobilisation, Hydrodynamique, Distribution spatiale, Sulfure, Processus syntectonique, Queensland.
- Wicri :
- topic : Ordinateur, Zinc, Plomb, Argent.
English descriptors
- KwdEn :
- Queensland Australia, base metals, computers, data processing, diagenesis, fault zones, faults, finite difference analysis, flow, genesis, hydrodynamics, inverse problem, lead, metals, mineralization, numerical models, remobilization, shale, siltstone, silver, spatial distribution, sulfides, syntectonic processes, three-dimensional models, zinc, zoning.
Abstract
This paper presents a combination of geometric reconstructions of the Century Zn-Pb-Ag deposit, and finite-difference modelling of coupled deformation and fluid flow. Our intention is to demonstrate that these computer-based applications represent a new approach in testing ore genesis models. We use a "visiometric" approach, utilising GoCad 3D structural and property modelling. Computer visualisation is applied to reveal metal zonations, fault distributions and timing, stratigraphic influence on zoning, and the nature and extent of metal redistribution during basin evolution and deformation. We also examine possible links between fluid flow, deformation, and mass transfer using the numerical code FLAC3D. Numerical modelling results suggest that subsurface fluid flow during basin inversion is compartmentalised, being focussed within more permeable fault zones, thus accounting for the secondary redistribution of base metals identified using the 3D reconstructions. However, the results do not explain the broad metal zonation observed. Both the spatial and numerical models suggest that Century is syngenetic, with further diagenesis and deformation producing 1-100 m-scale (re)mobilisation.
Affiliations:
Links toward previous steps (curation, corpus...)
Links to Exploration step
Pascal:09-0121431Le document en format XML
<record><TEI><teiHeader><fileDesc><titleStmt><title xml:lang="en" level="a">Modelling the giant, Zn-Pb-Ag Century deposit, Queensland, Australia</title><author><name sortKey="Feltrin, L" sort="Feltrin, L" uniqKey="Feltrin L" first="L." last="Feltrin">L. Feltrin</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Predictive Mineral Discovery Cooperative Research Centre, School of Earth Sciences, James Cook University</s1><s2>Queensland, 4811</s2><s3>AUS</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Australie</country><wicri:noRegion>Queensland, 4811</wicri:noRegion></affiliation></author><author><name sortKey="Mclellan, J G" sort="Mclellan, J G" uniqKey="Mclellan J" first="J. G." last="Mclellan">J. G. Mclellan</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Predictive Mineral Discovery Cooperative Research Centre, School of Earth Sciences, James Cook University</s1><s2>Queensland, 4811</s2><s3>AUS</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Australie</country><wicri:noRegion>Queensland, 4811</wicri:noRegion></affiliation></author><author><name sortKey="Oliver, N H S" sort="Oliver, N H S" uniqKey="Oliver N" first="N. H. S." last="Oliver">N. H. S. Oliver</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Predictive Mineral Discovery Cooperative Research Centre, School of Earth Sciences, James Cook University</s1><s2>Queensland, 4811</s2><s3>AUS</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Australie</country><wicri:noRegion>Queensland, 4811</wicri:noRegion></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">INIST</idno><idno type="inist">09-0121431</idno><date when="2009">2009</date><idno type="stanalyst">PASCAL 09-0121431 INIST</idno><idno type="RBID">Pascal:09-0121431</idno><idno type="wicri:Area/PascalFrancis/Corpus">002F77</idno><idno type="wicri:Area/PascalFrancis/Curation">003041</idno><idno type="wicri:Area/PascalFrancis/Checkpoint">002991</idno><idno type="wicri:explorRef" wicri:stream="PascalFrancis" wicri:step="Checkpoint">002991</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Modelling the giant, Zn-Pb-Ag Century deposit, Queensland, Australia</title><author><name sortKey="Feltrin, L" sort="Feltrin, L" uniqKey="Feltrin L" first="L." last="Feltrin">L. Feltrin</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Predictive Mineral Discovery Cooperative Research Centre, School of Earth Sciences, James Cook University</s1><s2>Queensland, 4811</s2><s3>AUS</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Australie</country><wicri:noRegion>Queensland, 4811</wicri:noRegion></affiliation></author><author><name sortKey="Mclellan, J G" sort="Mclellan, J G" uniqKey="Mclellan J" first="J. G." last="Mclellan">J. G. Mclellan</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Predictive Mineral Discovery Cooperative Research Centre, School of Earth Sciences, James Cook University</s1><s2>Queensland, 4811</s2><s3>AUS</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Australie</country><wicri:noRegion>Queensland, 4811</wicri:noRegion></affiliation></author><author><name sortKey="Oliver, N H S" sort="Oliver, N H S" uniqKey="Oliver N" first="N. H. S." last="Oliver">N. H. S. Oliver</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Predictive Mineral Discovery Cooperative Research Centre, School of Earth Sciences, James Cook University</s1><s2>Queensland, 4811</s2><s3>AUS</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Australie</country><wicri:noRegion>Queensland, 4811</wicri:noRegion></affiliation></author></analytic><series><title level="j" type="main">Computers & geosciences</title><title level="j" type="abbreviated">Comput. geosci.</title><idno type="ISSN">0098-3004</idno><imprint><date when="2009">2009</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Computers & geosciences</title><title level="j" type="abbreviated">Comput. geosci.</title><idno type="ISSN">0098-3004</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Queensland Australia</term><term>base metals</term><term>computers</term><term>data processing</term><term>diagenesis</term><term>fault zones</term><term>faults</term><term>finite difference analysis</term><term>flow</term><term>genesis</term><term>hydrodynamics</term><term>inverse problem</term><term>lead</term><term>metals</term><term>mineralization</term><term>numerical models</term><term>remobilization</term><term>shale</term><term>siltstone</term><term>silver</term><term>spatial distribution</term><term>sulfides</term><term>syntectonic processes</term><term>three-dimensional models</term><term>zinc</term><term>zoning</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Modèle numérique</term><term>Méthode différence finie</term><term>Siltstone</term><term>Ecoulement</term><term>Ordinateur</term><term>Minéralisation</term><term>Genèse</term><term>Elément métallique</term><term>Zonation</term><term>Faille</term><term>Shale</term><term>Problème inverse</term><term>Zone faillée</term><term>Métal base</term><term>Diagenèse</term><term>Traitement donnée</term><term>Modèle 3 dimensions</term><term>Zinc</term><term>Plomb</term><term>Argent</term><term>Remobilisation</term><term>Hydrodynamique</term><term>Distribution spatiale</term><term>Sulfure</term><term>Processus syntectonique</term><term>Queensland</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Ordinateur</term><term>Zinc</term><term>Plomb</term><term>Argent</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">This paper presents a combination of geometric reconstructions of the Century Zn-Pb-Ag deposit, and finite-difference modelling of coupled deformation and fluid flow. Our intention is to demonstrate that these computer-based applications represent a new approach in testing ore genesis models. We use a "visiometric" approach, utilising GoCad 3D structural and property modelling. Computer visualisation is applied to reveal metal zonations, fault distributions and timing, stratigraphic influence on zoning, and the nature and extent of metal redistribution during basin evolution and deformation. We also examine possible links between fluid flow, deformation, and mass transfer using the numerical code FLAC3D. Numerical modelling results suggest that subsurface fluid flow during basin inversion is compartmentalised, being focussed within more permeable fault zones, thus accounting for the secondary redistribution of base metals identified using the 3D reconstructions. However, the results do not explain the broad metal zonation observed. Both the spatial and numerical models suggest that Century is syngenetic, with further diagenesis and deformation producing 1-100 m-scale (re)mobilisation.</div></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0098-3004</s0></fA01><fA03 i2="1"><s0>Comput. geosci.</s0></fA03><fA05><s2>35</s2></fA05><fA06><s2>1</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>Modelling the giant, Zn-Pb-Ag Century deposit, Queensland, Australia</s1></fA08><fA09 i1="01" i2="1" l="ENG"><s1>Geological Survey of Canada</s1></fA09><fA11 i1="01" i2="1"><s1>FELTRIN (L.)</s1></fA11><fA11 i1="02" i2="1"><s1>MCLELLAN (J. G.)</s1></fA11><fA11 i1="03" i2="1"><s1>OLIVER (N. H. S.)</s1></fA11><fA12 i1="01" i2="1"><s1>ZANCHI (Andrea)</s1><s9>ed.</s9></fA12><fA12 i1="02" i2="1"><s1>DE DONATIS (Mauro)</s1><s9>ed.</s9></fA12><fA12 i1="03" i2="1"><s1>GIBBS (Alan)</s1><s9>ed.</s9></fA12><fA12 i1="04" i2="1"><s1>MALLET (Jean-Lauren)</s1><s9>ed.</s9></fA12><fA14 i1="01"><s1>Predictive Mineral Discovery Cooperative Research Centre, School of Earth Sciences, James Cook University</s1><s2>Queensland, 4811</s2><s3>AUS</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></fA14><fA15 i1="01"><s1>Dipartimento di Science, Geologiche e Geotecnologie, Universita degli studi di Milano-Bicocca, Piazza della Scienza 41</s1><s2>20126 Milan</s2><s3>ITA</s3><sZ>1 aut.</sZ></fA15><fA15 i1="02"><s1>Laboratory of Information-tech for Earth and Environmental Sciences, University of Urbino, Campus Scientifico</s1><s2>51029 Urbino</s2><s3>ITA</s3><sZ>2 aut.</sZ></fA15><fA15 i1="03"><s1>Midland Valley Exploration Ltd, 14 Park Circus</s1><s2>Glasgow G3 6AX</s2><s3>GBR</s3><sZ>3 aut.</sZ></fA15><fA15 i1="04"><s1>Ecole Nationale Politechnique Laurenne (ENPL)-Nancy, Rue du Doyen Marcel Roubault-BP 40</s1><s2>54500 Vandoeuvre</s2><s3>FRA</s3><sZ>4 aut.</sZ></fA15><fA20><s1>108-133</s1></fA20><fA21><s1>2009</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>17165</s2><s5>354000185036570070</s5></fA43><fA44><s0>0000</s0><s1>© 2009 INIST-CNRS. All rights reserved.</s1></fA44><fA45><s0>2 p.</s0></fA45><fA47 i1="01" i2="1"><s0>09-0121431</s0></fA47><fA60><s1>P</s1><s2>C</s2></fA60><fA61><s0>A</s0></fA61><fA64 i1="01" i2="1"><s0>Computers & geosciences</s0></fA64><fA66 i1="01"><s0>GBR</s0></fA66><fC01 i1="01" l="ENG"><s0>This paper presents a combination of geometric reconstructions of the Century Zn-Pb-Ag deposit, and finite-difference modelling of coupled deformation and fluid flow. Our intention is to demonstrate that these computer-based applications represent a new approach in testing ore genesis models. We use a "visiometric" approach, utilising GoCad 3D structural and property modelling. Computer visualisation is applied to reveal metal zonations, fault distributions and timing, stratigraphic influence on zoning, and the nature and extent of metal redistribution during basin evolution and deformation. We also examine possible links between fluid flow, deformation, and mass transfer using the numerical code FLAC3D. Numerical modelling results suggest that subsurface fluid flow during basin inversion is compartmentalised, being focussed within more permeable fault zones, thus accounting for the secondary redistribution of base metals identified using the 3D reconstructions. However, the results do not explain the broad metal zonation observed. Both the spatial and numerical models suggest that Century is syngenetic, with further diagenesis and deformation producing 1-100 m-scale (re)mobilisation.</s0></fC01><fC02 i1="01" i2="2"><s0>001E01E02</s0></fC02><fC02 i1="02" i2="2"><s0>001E01L</s0></fC02><fC02 i1="03" i2="2"><s0>221A02</s0></fC02><fC02 i1="04" i2="2"><s0>225A</s0></fC02><fC03 i1="01" i2="2" l="FRE"><s0>Modèle numérique</s0><s5>01</s5></fC03><fC03 i1="01" i2="2" l="ENG"><s0>numerical models</s0><s5>01</s5></fC03><fC03 i1="02" i2="2" l="FRE"><s0>Méthode différence finie</s0><s5>02</s5></fC03><fC03 i1="02" i2="2" l="ENG"><s0>finite difference analysis</s0><s5>02</s5></fC03><fC03 i1="03" i2="2" l="FRE"><s0>Siltstone</s0><s2>NV</s2><s5>03</s5></fC03><fC03 i1="03" i2="2" l="ENG"><s0>siltstone</s0><s2>NV</s2><s5>03</s5></fC03><fC03 i1="03" i2="2" l="SPA"><s0>Siliston</s0><s2>NV</s2><s5>03</s5></fC03><fC03 i1="04" i2="2" l="FRE"><s0>Ecoulement</s0><s5>04</s5></fC03><fC03 i1="04" i2="2" l="ENG"><s0>flow</s0><s5>04</s5></fC03><fC03 i1="05" i2="2" l="FRE"><s0>Ordinateur</s0><s5>05</s5></fC03><fC03 i1="05" i2="2" l="ENG"><s0>computers</s0><s5>05</s5></fC03><fC03 i1="05" i2="2" l="SPA"><s0>Computadora</s0><s5>05</s5></fC03><fC03 i1="06" i2="2" l="FRE"><s0>Minéralisation</s0><s5>06</s5></fC03><fC03 i1="06" i2="2" l="ENG"><s0>mineralization</s0><s5>06</s5></fC03><fC03 i1="06" i2="2" l="SPA"><s0>Mineralización</s0><s5>06</s5></fC03><fC03 i1="07" i2="2" l="FRE"><s0>Genèse</s0><s5>07</s5></fC03><fC03 i1="07" i2="2" l="ENG"><s0>genesis</s0><s5>07</s5></fC03><fC03 i1="07" i2="2" l="SPA"><s0>Génesis</s0><s5>07</s5></fC03><fC03 i1="08" i2="2" l="FRE"><s0>Elément métallique</s0><s5>08</s5></fC03><fC03 i1="08" i2="2" l="ENG"><s0>metals</s0><s5>08</s5></fC03><fC03 i1="08" i2="2" l="SPA"><s0>Elemento metálico</s0><s5>08</s5></fC03><fC03 i1="09" i2="2" l="FRE"><s0>Zonation</s0><s5>09</s5></fC03><fC03 i1="09" i2="2" l="ENG"><s0>zoning</s0><s5>09</s5></fC03><fC03 i1="09" i2="2" l="SPA"><s0>Zonalidad</s0><s5>09</s5></fC03><fC03 i1="10" i2="2" l="FRE"><s0>Faille</s0><s5>10</s5></fC03><fC03 i1="10" i2="2" l="ENG"><s0>faults</s0><s5>10</s5></fC03><fC03 i1="10" i2="2" l="SPA"><s0>Quebrado</s0><s5>10</s5></fC03><fC03 i1="11" i2="2" l="FRE"><s0>Shale</s0><s2>NV</s2><s5>11</s5></fC03><fC03 i1="11" i2="2" l="ENG"><s0>shale</s0><s2>NV</s2><s5>11</s5></fC03><fC03 i1="11" i2="2" l="SPA"><s0>Esquisto</s0><s2>NV</s2><s5>11</s5></fC03><fC03 i1="12" i2="2" l="FRE"><s0>Problème inverse</s0><s5>12</s5></fC03><fC03 i1="12" i2="2" l="ENG"><s0>inverse problem</s0><s5>12</s5></fC03><fC03 i1="12" i2="2" l="SPA"><s0>Problema inverso</s0><s5>12</s5></fC03><fC03 i1="13" i2="2" l="FRE"><s0>Zone faillée</s0><s5>13</s5></fC03><fC03 i1="13" i2="2" l="ENG"><s0>fault zones</s0><s5>13</s5></fC03><fC03 i1="13" i2="2" l="SPA"><s0>Zona falla</s0><s5>13</s5></fC03><fC03 i1="14" i2="2" l="FRE"><s0>Métal base</s0><s5>14</s5></fC03><fC03 i1="14" i2="2" l="ENG"><s0>base metals</s0><s5>14</s5></fC03><fC03 i1="14" i2="2" l="SPA"><s0>Metales base</s0><s5>14</s5></fC03><fC03 i1="15" i2="2" l="FRE"><s0>Diagenèse</s0><s5>15</s5></fC03><fC03 i1="15" i2="2" l="ENG"><s0>diagenesis</s0><s5>15</s5></fC03><fC03 i1="15" i2="2" l="SPA"><s0>Diagénesis</s0><s5>15</s5></fC03><fC03 i1="16" i2="2" l="FRE"><s0>Traitement donnée</s0><s5>16</s5></fC03><fC03 i1="16" i2="2" l="ENG"><s0>data processing</s0><s5>16</s5></fC03><fC03 i1="16" i2="2" l="SPA"><s0>Tratamiento datos</s0><s5>16</s5></fC03><fC03 i1="17" i2="2" l="FRE"><s0>Modèle 3 dimensions</s0><s5>17</s5></fC03><fC03 i1="17" i2="2" l="ENG"><s0>three-dimensional models</s0><s5>17</s5></fC03><fC03 i1="17" i2="2" l="SPA"><s0>Modelo 3 dimensiones</s0><s5>17</s5></fC03><fC03 i1="18" i2="2" l="FRE"><s0>Zinc</s0><s5>18</s5></fC03><fC03 i1="18" i2="2" l="ENG"><s0>zinc</s0><s5>18</s5></fC03><fC03 i1="18" i2="2" l="SPA"><s0>Zinc</s0><s5>18</s5></fC03><fC03 i1="19" i2="2" l="FRE"><s0>Plomb</s0><s5>19</s5></fC03><fC03 i1="19" i2="2" l="ENG"><s0>lead</s0><s5>19</s5></fC03><fC03 i1="19" i2="2" l="SPA"><s0>Plomo</s0><s5>19</s5></fC03><fC03 i1="20" i2="2" l="FRE"><s0>Argent</s0><s5>20</s5></fC03><fC03 i1="20" i2="2" l="ENG"><s0>silver</s0><s5>20</s5></fC03><fC03 i1="20" i2="2" l="SPA"><s0>Plata</s0><s5>20</s5></fC03><fC03 i1="21" i2="2" l="FRE"><s0>Remobilisation</s0><s5>21</s5></fC03><fC03 i1="21" i2="2" l="ENG"><s0>remobilization</s0><s5>21</s5></fC03><fC03 i1="21" i2="2" l="SPA"><s0>Remobilización</s0><s5>21</s5></fC03><fC03 i1="22" i2="2" l="FRE"><s0>Hydrodynamique</s0><s5>22</s5></fC03><fC03 i1="22" i2="2" l="ENG"><s0>hydrodynamics</s0><s5>22</s5></fC03><fC03 i1="22" i2="2" l="SPA"><s0>Hidrodinámica</s0><s5>22</s5></fC03><fC03 i1="23" i2="2" l="FRE"><s0>Distribution spatiale</s0><s5>23</s5></fC03><fC03 i1="23" i2="2" l="ENG"><s0>spatial distribution</s0><s5>23</s5></fC03><fC03 i1="23" i2="2" l="SPA"><s0>Distribución espacial</s0><s5>23</s5></fC03><fC03 i1="24" i2="2" l="FRE"><s0>Sulfure</s0><s2>NZ</s2><s5>24</s5></fC03><fC03 i1="24" i2="2" l="ENG"><s0>sulfides</s0><s2>NZ</s2><s5>24</s5></fC03><fC03 i1="24" i2="2" l="SPA"><s0>Sulfuro</s0><s2>NZ</s2><s5>24</s5></fC03><fC03 i1="25" i2="2" l="FRE"><s0>Processus syntectonique</s0><s5>25</s5></fC03><fC03 i1="25" i2="2" l="ENG"><s0>syntectonic processes</s0><s5>25</s5></fC03><fC03 i1="25" i2="2" l="SPA"><s0>Proceso sintectónico</s0><s5>25</s5></fC03><fC03 i1="26" i2="2" l="FRE"><s0>Queensland</s0><s2>NG</s2><s5>61</s5></fC03><fC03 i1="26" i2="2" l="ENG"><s0>Queensland Australia</s0><s2>NG</s2><s5>61</s5></fC03><fC03 i1="26" i2="2" l="SPA"><s0>Queensland</s0><s2>NG</s2><s5>61</s5></fC03><fC07 i1="01" i2="2" l="FRE"><s0>Roche clastique</s0><s2>NV</s2></fC07><fC07 i1="01" i2="2" l="ENG"><s0>clastic rocks</s0><s2>NV</s2></fC07><fC07 i1="01" i2="2" l="SPA"><s0>Roca clástica</s0><s2>NV</s2></fC07><fC07 i1="02" i2="2" l="FRE"><s0>Roche sédimentaire</s0><s2>NV</s2></fC07><fC07 i1="02" i2="2" l="ENG"><s0>sedimentary rocks</s0><s2>NV</s2></fC07><fC07 i1="02" i2="2" l="SPA"><s0>Roca sedimentaria</s0><s2>NV</s2></fC07><fC07 i1="03" i2="2" l="FRE"><s0>Australie</s0><s2>NG</s2></fC07><fC07 i1="03" i2="2" l="ENG"><s0>Australia</s0><s2>NG</s2></fC07><fC07 i1="03" i2="2" l="SPA"><s0>Australia</s0><s2>NG</s2></fC07><fC07 i1="04" i2="2" l="FRE"><s0>Australasie</s0></fC07><fC07 i1="04" i2="2" l="ENG"><s0>Australasia</s0></fC07><fC07 i1="04" i2="2" l="SPA"><s0>Australasia</s0></fC07><fN21><s1>082</s1></fN21></pA><pR><fA30 i1="01" i2="1" l="ENG"><s1>The Renaissance of Geology. IGC</s1><s2>32</s2><s3>Florence ITA</s3><s4>2004</s4></fA30></pR></standard></inist><affiliations><list><country><li>Australie</li></country></list><tree><country name="Australie"><noRegion><name sortKey="Feltrin, L" sort="Feltrin, L" uniqKey="Feltrin L" first="L." last="Feltrin">L. Feltrin</name></noRegion><name sortKey="Mclellan, J G" sort="Mclellan, J G" uniqKey="Mclellan J" first="J. G." last="Mclellan">J. G. Mclellan</name><name sortKey="Oliver, N H S" sort="Oliver, N H S" uniqKey="Oliver N" first="N. H. S." last="Oliver">N. H. S. Oliver</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Asie/explor/AustralieFrV1/Data/PascalFrancis/Checkpoint
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 002991 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/PascalFrancis/Checkpoint/biblio.hfd -nk 002991 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= Wicri/Asie
|area= AustralieFrV1
|flux= PascalFrancis
|étape= Checkpoint
|type= RBID
|clé= Pascal:09-0121431
|texte= Modelling the giant, Zn-Pb-Ag Century deposit, Queensland, Australia
}}
| This area was generated with Dilib version V0.6.33. |  |