Quartz vein morphology and implications for formation depth and classification of Archaean gold-vein deposits
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A simplified scheme to categorise quartz vein morphology from gold deposits is based on the growth direction of quartz or pseudomorphed chalcedony in the veins. The categories are scale-independent and are: (1) face-control, (2) displacement-control, (3) parallel-control, (4) radiating, (5) non-directional control, (6) replacement, and (7) modified. Quartz vein textures do not indicate any particular type of mineralisation. For the depth continuum of Archaean lode-gold deposits of the Yilgarn Craton all seven categories of texture are variously present. However, crustal depth is a major control. Parallel and radiating textures are characteristic of gold deposits formed at the near surface; displacement and non-directional control are typical of deposits at midcrustal (greenschist and amphibolite) conditions; and face-control shows a range of conditions from the near surface to midcrustal. Replacement and modified textures embrace a wide variety of alteration and deformation conditions, and can occur in gold deposits at all crustal levels.
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<record><TEI><teiHeader><fileDesc><titleStmt><title>Quartz vein morphology and implications for formation depth and classification of Archaean gold-vein deposits</title><author><name sortKey="Vearncombe, J R" uniqKey="Vearncombe J">J.R. Vearncombe</name><affiliation wicri:level="1"><mods:affiliation>Key Centre for Teaching and Research in Strategic Mineral Deposits, Department of Geology, The University of Western Australia, Nedlands 6009, Australia</mods:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>Key Centre for Teaching and Research in Strategic Mineral Deposits, Department of Geology, The University of Western Australia, Nedlands 6009</wicri:regionArea></affiliation></author></titleStmt><publicationStmt><idno type="RBID">ISTEX:539FD3076E6684FB009031DDD7B8629B2E4D93AC</idno><date when="1993">1993</date><idno type="doi">10.1016/0169-1368(93)90036-X</idno><idno type="url">https://api.istex.fr/document/539FD3076E6684FB009031DDD7B8629B2E4D93AC/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">002268</idno><idno type="wicri:Area/Istex/Curation">002268</idno></publicationStmt><seriesStmt><idno type="ISSN">0169-1368</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="eng">A simplified scheme to categorise quartz vein morphology from gold deposits is based on the growth direction of quartz or pseudomorphed chalcedony in the veins. The categories are scale-independent and are: (1) face-control, (2) displacement-control, (3) parallel-control, (4) radiating, (5) non-directional control, (6) replacement, and (7) modified. Quartz vein textures do not indicate any particular type of mineralisation. For the depth continuum of Archaean lode-gold deposits of the Yilgarn Craton all seven categories of texture are variously present. However, crustal depth is a major control. Parallel and radiating textures are characteristic of gold deposits formed at the near surface; displacement and non-directional control are typical of deposits at midcrustal (greenschist and amphibolite) conditions; and face-control shows a range of conditions from the near surface to midcrustal. Replacement and modified textures embrace a wide variety of alteration and deformation conditions, and can occur in gold deposits at all crustal levels. </div></front></TEI><istex><corpusName>elsevier</corpusName><copyrightdate>1993</copyrightdate><author><json:item><name>J.R. Vearncombe</name><affiliations><json:string>Key Centre for Teaching and Research in Strategic Mineral Deposits, Department of Geology, The University of Western Australia, Nedlands 6009, Australia</json:string></affiliations></json:item></author><language></language><abstract>A simplified scheme to categorise quartz vein morphology from gold deposits is based on the growth direction of quartz or pseudomorphed chalcedony in the veins. The categories are scale-independent and are: (1) face-control, (2) displacement-control, (3) parallel-control, (4) radiating, (5) non-directional control, (6) replacement, and (7) modified. Quartz vein textures do not indicate any particular type of mineralisation. For the depth continuum of Archaean lode-gold deposits of the Yilgarn Craton all seven categories of texture are variously present. However, crustal depth is a major control. Parallel and radiating textures are characteristic of gold deposits formed at the near surface; displacement and non-directional control are typical of deposits at midcrustal (greenschist and amphibolite) conditions; and face-control shows a range of conditions from the near surface to midcrustal. Replacement and modified textures embrace a wide variety of alteration and deformation conditions, and can occur in gold deposits at all crustal levels.</abstract><title>Quartz vein morphology and implications for formation depth and classification of Archaean gold-vein deposits</title><pii><json:string>0169-1368(93)90036-X</json:string></pii><genre></genre><serie><genre><json:string>Book</json:string></genre><language></language><title>Unpubl. B.Sc. 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The categories are scale-independent and are: (1) face-control, (2) displacement-control, (3) parallel-control, (4) radiating, (5) non-directional control, (6) replacement, and (7) modified. Quartz vein textures do not indicate any particular type of mineralisation. For the depth continuum of Archaean lode-gold deposits of the Yilgarn Craton all seven categories of texture are variously present. However, crustal depth is a major control. Parallel and radiating textures are characteristic of gold deposits formed at the near surface; displacement and non-directional control are typical of deposits at midcrustal (greenschist and amphibolite) conditions; and face-control shows a range of conditions from the near surface to midcrustal. Replacement and modified textures embrace a wide variety of alteration and deformation conditions, and can occur in gold deposits at all crustal levels.</p></abstract></profileDesc><revisionDesc><change when="1992-08-03">Received</change><change when="1993-01-13">Registration</change><change when="1993">Published</change></revisionDesc></teiHeader></istex:fulltextTEI></fulltext><metadata><istex:metadataXml wicri:clean="Elsevier converted-article found"><istex:xmlDeclaration>version="1.0" encoding="utf-8"</istex:xmlDeclaration><istex:docType PUBLIC="-//ES//DTD journal article DTD version 4.5.2//EN//XML" URI="art452.dtd" name="istex:docType"></istex:docType><istex:document><converted-article version="4.5.2" docsubtype="fla"><item-info><jid>OREGEO</jid><aid>9390036X</aid><ce:pii>0169-1368(93)90036-X</ce:pii><ce:doi>10.1016/0169-1368(93)90036-X</ce:doi><ce:copyright type="unknown" year="1993"></ce:copyright></item-info><head><ce:dochead><ce:textfn>Research paper</ce:textfn></ce:dochead><ce:title>Quartz vein morphology and implications for formation depth and classification of Archaean gold-vein deposits</ce:title><ce:author-group><ce:author><ce:given-name>J.R.</ce:given-name><ce:surname>Vearncombe</ce:surname></ce:author><ce:affiliation><ce:textfn>Key Centre for Teaching and Research in Strategic Mineral Deposits, Department of Geology, The University of Western Australia, Nedlands 6009, Australia</ce:textfn></ce:affiliation></ce:author-group><ce:date-received day="3" month="8" year="1992"></ce:date-received><ce:date-accepted day="13" month="1" year="1993"></ce:date-accepted><ce:abstract><ce:section-title>Abstract</ce:section-title><ce:abstract-sec><ce:simple-para>A simplified scheme to categorise quartz vein morphology from gold deposits is based on the growth direction of quartz or pseudomorphed chalcedony in the veins. The categories are scale-independent and are: (1) face-control, (2) displacement-control, (3) parallel-control, (4) radiating, (5) non-directional control, (6) replacement, and (7) modified. Quartz vein textures do not indicate any particular type of mineralisation. For the depth continuum of Archaean lode-gold deposits of the Yilgarn Craton all seven categories of texture are variously present. However, crustal depth is a major control. Parallel and radiating textures are characteristic of gold deposits formed at the near surface; displacement and non-directional control are typical of deposits at midcrustal (greenschist and amphibolite) conditions; and face-control shows a range of conditions from the near surface to midcrustal. Replacement and modified textures embrace a wide variety of alteration and deformation conditions, and can occur in gold deposits at all crustal levels.</ce:simple-para></ce:abstract-sec></ce:abstract></head></converted-article></istex:document></istex:metadataXml><mods version="3.5"><titleInfo><title>Quartz vein morphology and implications for formation depth and classification of Archaean gold-vein deposits</title></titleInfo><titleInfo type="alternative"><title>Quartz vein morphology and implications for formation depth and classification of Archaean gold-vein deposits</title></titleInfo><name type="personal"><namePart type="given">J.R.</namePart><namePart type="family">Vearncombe</namePart><affiliation>Key Centre for Teaching and Research in Strategic Mineral Deposits, Department of Geology, The University of Western Australia, Nedlands 6009, Australia</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><originInfo><publisher>ELSEVIER</publisher><dateIssued encoding="w3cdtf">1993</dateIssued><dateCaptured encoding="w3cdtf">1992-08-03</dateCaptured><dateValid encoding="w3cdtf">1993-01-13</dateValid><copyrightDate encoding="w3cdtf">1993</copyrightDate></originInfo><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="eng">A simplified scheme to categorise quartz vein morphology from gold deposits is based on the growth direction of quartz or pseudomorphed chalcedony in the veins. The categories are scale-independent and are: (1) face-control, (2) displacement-control, (3) parallel-control, (4) radiating, (5) non-directional control, (6) replacement, and (7) modified. Quartz vein textures do not indicate any particular type of mineralisation. For the depth continuum of Archaean lode-gold deposits of the Yilgarn Craton all seven categories of texture are variously present. However, crustal depth is a major control. Parallel and radiating textures are characteristic of gold deposits formed at the near surface; displacement and non-directional control are typical of deposits at midcrustal (greenschist and amphibolite) conditions; and face-control shows a range of conditions from the near surface to midcrustal. Replacement and modified textures embrace a wide variety of alteration and deformation conditions, and can occur in gold deposits at all crustal levels. </abstract><note type="content">Section title: Research paper</note><relatedItem type="host"><titleInfo><title>Ore Geology Reviews</title></titleInfo><titleInfo type="abbreviated"><title>OREGEO</title></titleInfo><originInfo><dateIssued encoding="w3cdtf">199309</dateIssued></originInfo><identifier type="ISSN">0169-1368</identifier><identifier type="PII">S0169-1368(00)X0060-1</identifier><part><date>1993</date><detail type="volume"><number>8</number><caption>vol.</caption></detail><detail type="issue"><number>5</number><caption>no.</caption></detail><extent unit="issue pages"><start>383</start><end>450</end></extent></part></relatedItem><relatedItem type="references" displayLabel="BIB1"><titleInfo><title>A microscopic study of vein quartz</title></titleInfo><name type="personal"><namePart type="given">S.F.</namePart><namePart type="family">Adams</namePart><role><roleTerm type="text">author</roleTerm></role></name><note>Adams, 1920</note><relatedItem type="host"><titleInfo><title>Econ. 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|clé= ISTEX:539FD3076E6684FB009031DDD7B8629B2E4D93AC
|texte= Quartz vein morphology and implications for formation depth and classification of Archaean gold-vein deposits
}}
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