Distribution of indium in the Animas - Chocaya - Siete Suyos District

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The Ánimas-Chocaya-Siete Suyos district in SW Bolivia hosts a Bolivian-type polymetallic vein mineralization composed mostly of cassiterite, sphalerite, pyrite, galena, stannite, lead sulfosalts, tin sulfosalts and silver sulfosalts. In addition to base (Zn, Sn, Pb) and precious (Ag) metals, importa...

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Detalles Bibliográficos
Autores: Martinez, Malena Cazorla, Tarres, Marta, Gemmrich, Laura, Torres, Belen, Artiaga, David, Martinez, Alvaro, Mollinedo, Diva, Caries Melgarejo, Joan, Torro, Lisard, Arce, Osvado, Alfonso, Pura
Formato: artículo
Fecha de Publicación:2019
Institución:Consejo Nacional de Ciencia Tecnología e Innovación
Repositorio:CONCYTEC-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.concytec.gob.pe:20.500.12390/2829
Enlace del recurso:https://hdl.handle.net/20.500.12390/2829
Nivel de acceso:acceso abierto
Materia:Sphalerite
Indium
Andes
https://purl.org/pe-repo/ocde/ford#1.05.02
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oai_identifier_str oai:repositorio.concytec.gob.pe:20.500.12390/2829
network_acronym_str CONC
network_name_str CONCYTEC-Institucional
repository_id_str 4689
dc.title.none.fl_str_mv Distribution of indium in the Animas - Chocaya - Siete Suyos District
title Distribution of indium in the Animas - Chocaya - Siete Suyos District
spellingShingle Distribution of indium in the Animas - Chocaya - Siete Suyos District
Martinez, Malena Cazorla
Sphalerite
Indium
Indium
Andes
https://purl.org/pe-repo/ocde/ford#1.05.02
title_short Distribution of indium in the Animas - Chocaya - Siete Suyos District
title_full Distribution of indium in the Animas - Chocaya - Siete Suyos District
title_fullStr Distribution of indium in the Animas - Chocaya - Siete Suyos District
title_full_unstemmed Distribution of indium in the Animas - Chocaya - Siete Suyos District
title_sort Distribution of indium in the Animas - Chocaya - Siete Suyos District
author Martinez, Malena Cazorla
author_facet Martinez, Malena Cazorla
Tarres, Marta
Gemmrich, Laura
Torres, Belen
Artiaga, David
Martinez, Alvaro
Mollinedo, Diva
Caries Melgarejo, Joan
Torro, Lisard
Arce, Osvado
Alfonso, Pura
author_role author
author2 Tarres, Marta
Gemmrich, Laura
Torres, Belen
Artiaga, David
Martinez, Alvaro
Mollinedo, Diva
Caries Melgarejo, Joan
Torro, Lisard
Arce, Osvado
Alfonso, Pura
author2_role author
author
author
author
author
author
author
author
author
author
dc.contributor.author.fl_str_mv Martinez, Malena Cazorla
Tarres, Marta
Gemmrich, Laura
Torres, Belen
Artiaga, David
Martinez, Alvaro
Mollinedo, Diva
Caries Melgarejo, Joan
Torro, Lisard
Arce, Osvado
Alfonso, Pura
dc.subject.none.fl_str_mv Sphalerite
topic Sphalerite
Indium
Indium
Andes
https://purl.org/pe-repo/ocde/ford#1.05.02
dc.subject.es_PE.fl_str_mv Indium
Indium
Andes
dc.subject.ocde.none.fl_str_mv https://purl.org/pe-repo/ocde/ford#1.05.02
description The Ánimas-Chocaya-Siete Suyos district in SW Bolivia hosts a Bolivian-type polymetallic vein mineralization composed mostly of cassiterite, sphalerite, pyrite, galena, stannite, lead sulfosalts, tin sulfosalts and silver sulfosalts. In addition to base (Zn, Sn, Pb) and precious (Ag) metals, important concentrations of In have been described. Systematic EPMA analyses have revealed that the highest concentrations are found in an early generation of sphalerite (up to 9.66 wt% In) and in stannite (up to 4.11 wt% In). Although In-bearing sphalerites are relatively Fe-rich (mostly between 6.0 and 18.1 mol % FeS), the atomic concentrations of these two elements do not yield any correlation. In contrast, In is positively correlated with Cu mostly along a Cu/In = 1 proportion pointing to a (In 3+ + Cu +) -> 2Zn 2+ coupled substitution. A relatively high activity of Cu during the crystallization of In-rich sphalerite is also supported by exsolutions of chalcopyrite and stannite.
publishDate 2019
dc.date.accessioned.none.fl_str_mv 2024-05-30T23:13:38Z
dc.date.available.none.fl_str_mv 2024-05-30T23:13:38Z
dc.date.issued.fl_str_mv 2019
dc.type.none.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12390/2829
url https://hdl.handle.net/20.500.12390/2829
dc.language.iso.none.fl_str_mv eng
language eng
dc.relation.ispartof.none.fl_str_mv LIFE WITH ORE DEPOSITS ON EARTH, PROCEEDINGS OF THE 15TH SGA BIENNIAL MEETING, 2019, VOLS 1-4
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Society of Geology Applied to Mineral Deposits
publisher.none.fl_str_mv Society of Geology Applied to Mineral Deposits
dc.source.none.fl_str_mv reponame:CONCYTEC-Institucional
instname:Consejo Nacional de Ciencia Tecnología e Innovación
instacron:CONCYTEC
instname_str Consejo Nacional de Ciencia Tecnología e Innovación
instacron_str CONCYTEC
institution CONCYTEC
reponame_str CONCYTEC-Institucional
collection CONCYTEC-Institucional
repository.name.fl_str_mv Repositorio Institucional CONCYTEC
repository.mail.fl_str_mv repositorio@concytec.gob.pe
_version_ 1844883054175191040
spelling Publicationrp07683600rp07671600rp07660600rp07672600rp07668600rp07667600rp07664600rp07669600rp07661600rp07682600rp07673600Martinez, Malena CazorlaTarres, MartaGemmrich, LauraTorres, BelenArtiaga, DavidMartinez, AlvaroMollinedo, DivaCaries Melgarejo, JoanTorro, LisardArce, OsvadoAlfonso, Pura2024-05-30T23:13:38Z2024-05-30T23:13:38Z2019https://hdl.handle.net/20.500.12390/2829The Ánimas-Chocaya-Siete Suyos district in SW Bolivia hosts a Bolivian-type polymetallic vein mineralization composed mostly of cassiterite, sphalerite, pyrite, galena, stannite, lead sulfosalts, tin sulfosalts and silver sulfosalts. In addition to base (Zn, Sn, Pb) and precious (Ag) metals, important concentrations of In have been described. Systematic EPMA analyses have revealed that the highest concentrations are found in an early generation of sphalerite (up to 9.66 wt% In) and in stannite (up to 4.11 wt% In). Although In-bearing sphalerites are relatively Fe-rich (mostly between 6.0 and 18.1 mol % FeS), the atomic concentrations of these two elements do not yield any correlation. In contrast, In is positively correlated with Cu mostly along a Cu/In = 1 proportion pointing to a (In 3+ + Cu +) -> 2Zn 2+ coupled substitution. A relatively high activity of Cu during the crystallization of In-rich sphalerite is also supported by exsolutions of chalcopyrite and stannite.Consejo Nacional de Ciencia, Tecnología e Innovación Tecnológica - ConcytecengSociety of Geology Applied to Mineral DepositsLIFE WITH ORE DEPOSITS ON EARTH, PROCEEDINGS OF THE 15TH SGA BIENNIAL MEETING, 2019, VOLS 1-4info:eu-repo/semantics/openAccessSphaleriteIndium-1Indium-1Andes-1https://purl.org/pe-repo/ocde/ford#1.05.02-1Distribution of indium in the Animas - Chocaya - Siete Suyos Districtinfo:eu-repo/semantics/articlereponame:CONCYTEC-Institucionalinstname:Consejo Nacional de Ciencia Tecnología e Innovacióninstacron:CONCYTEC20.500.12390/2829oai:repositorio.concytec.gob.pe:20.500.12390/28292024-05-30 16:11:49.522http://purl.org/coar/access_right/c_14cbinfo:eu-repo/semantics/closedAccessmetadata only accesshttps://repositorio.concytec.gob.peRepositorio Institucional CONCYTECrepositorio@concytec.gob.pe#PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE#<Publication xmlns="https://www.openaire.eu/cerif-profile/1.1/" id="0ccf1505-cab1-4ec2-bc80-14782795d980"> <Type xmlns="https://www.openaire.eu/cerif-profile/vocab/COAR_Publication_Types">http://purl.org/coar/resource_type/c_1843</Type> <Language>eng</Language> <Title>Distribution of indium in the Animas - Chocaya - Siete Suyos District</Title> <PublishedIn> <Publication> <Title>LIFE WITH ORE DEPOSITS ON EARTH, PROCEEDINGS OF THE 15TH SGA BIENNIAL MEETING, 2019, VOLS 1-4</Title> </Publication> </PublishedIn> <PublicationDate>2019</PublicationDate> <Authors> <Author> <DisplayName>Martinez, Malena Cazorla</DisplayName> <Person id="rp07683" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Tarres, Marta</DisplayName> <Person id="rp07671" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Gemmrich, Laura</DisplayName> <Person id="rp07660" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Torres, Belen</DisplayName> <Person id="rp07672" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Artiaga, David</DisplayName> <Person id="rp07668" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Martinez, Alvaro</DisplayName> <Person id="rp07667" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Mollinedo, Diva</DisplayName> <Person id="rp07664" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Caries Melgarejo, Joan</DisplayName> <Person id="rp07669" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Torro, Lisard</DisplayName> <Person id="rp07661" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Arce, Osvado</DisplayName> <Person id="rp07682" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Alfonso, Pura</DisplayName> <Person id="rp07673" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> </Authors> <Editors> </Editors> <Publishers> <Publisher> <DisplayName>Society of Geology Applied to Mineral Deposits</DisplayName> <OrgUnit /> </Publisher> </Publishers> <Keyword>Sphalerite</Keyword> <Keyword>Indium</Keyword> <Keyword>Indium</Keyword> <Keyword>Andes</Keyword> <Abstract>The Ánimas-Chocaya-Siete Suyos district in SW Bolivia hosts a Bolivian-type polymetallic vein mineralization composed mostly of cassiterite, sphalerite, pyrite, galena, stannite, lead sulfosalts, tin sulfosalts and silver sulfosalts. In addition to base (Zn, Sn, Pb) and precious (Ag) metals, important concentrations of In have been described. Systematic EPMA analyses have revealed that the highest concentrations are found in an early generation of sphalerite (up to 9.66 wt% In) and in stannite (up to 4.11 wt% In). Although In-bearing sphalerites are relatively Fe-rich (mostly between 6.0 and 18.1 mol % FeS), the atomic concentrations of these two elements do not yield any correlation. In contrast, In is positively correlated with Cu mostly along a Cu/In = 1 proportion pointing to a (In 3+ + Cu +) -&gt; 2Zn 2+ coupled substitution. A relatively high activity of Cu during the crystallization of In-rich sphalerite is also supported by exsolutions of chalcopyrite and stannite.</Abstract> <Access xmlns="http://purl.org/coar/access_right" > </Access> </Publication> -1
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