EVALUACIÓN GEOQUÍMICA DE RESIDUOS MINEROS (JALES OCOLAS) DE MINERALIZACIÓN DE TIPO EPITERMAL, HIDALGO, MÉXICO
He mining district Pachuca-Real del Monte is located to the center-east of Mexico, between the geographical coordinates 20°07’30” of north latitude and 98°44 ‘00 “ of length west. The residues are derived from an epithermal mineralization. Concentrations of Pb and the Mn are significant. The mineral...
| Autores: | , , |
|---|---|
| Formato: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2009 |
| País: | México |
| Recursos: | Universidad Autónoma de San Luis Potosí |
| Repositorio: | Redalyc-UASLP |
| OAI Identifier: | oai:redalyc.org:45437348007 |
| Acesso em linha: | https://www.redalyc.org/articulo.oa?id=45437348007 |
| Access Level: | acceso abierto |
| Palavra-chave: | Geología México tailings epithermal neoformation Mining district |
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EVALUACIÓN GEOQUÍMICA DE RESIDUOS MINEROS (JALES OCOLAS) DE MINERALIZACIÓN DE TIPO EPITERMAL, HIDALGO, MÉXICORaúl MorenoMarcos G. MonroyE. Pedro CastañedaGeologíaMéxicotailingsepithermalneoformationMining districtHe mining district Pachuca-Real del Monte is located to the center-east of Mexico, between the geographical coordinates 20°07’30” of north latitude and 98°44 ‘00 “ of length west. The residues are derived from an epithermal mineralization. Concentrations of Pb and the Mn are significant. The mineralization consists of pyrite, limonite-goethite-hematite, sphalerite, galena, and chalcopyrite associated with quartz, calcite and silicates. X-rays diffraction patterns determined quartz as the mayor mineral phase, with minor gypsum, calcite, alunite, and pyrite. The statistical analysis showed the frequent association of Zn-Cd. The microanalysis with the scanning electronic microscope and electronic microprobe showed the neoformation of the pyrite and the oxidation and precipitate of sulfides. The tests NOM-053 and EPA-1312 showed that the Cd, Ni, Ag, Pb Mn, Zn, and As do not exceed the LMP. Only the Pb is superior to the LMP in the first test. These residues might be classified as dangerous with regard to the Pb.Universidad de Costa Rica2009info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdf0256-7024https://www.redalyc.org/articulo.oa?id=45437348007Revista Geológica de América Central (Costa Rica) Num.41reponame:Redalyc-UASLPinstname:Universidad Autónoma de San Luis Potosíinstacron:UASLPeshttp://www.redalyc.org/revista.oa?id=454Revista Geológica de América Centralinfo:eu-repo/semantics/openAccessoai:redalyc.org:454373480072024-08-23T15:33:43Z |
| dc.title.none.fl_str_mv |
EVALUACIÓN GEOQUÍMICA DE RESIDUOS MINEROS (JALES OCOLAS) DE MINERALIZACIÓN DE TIPO EPITERMAL, HIDALGO, MÉXICO |
| title |
EVALUACIÓN GEOQUÍMICA DE RESIDUOS MINEROS (JALES OCOLAS) DE MINERALIZACIÓN DE TIPO EPITERMAL, HIDALGO, MÉXICO |
| spellingShingle |
EVALUACIÓN GEOQUÍMICA DE RESIDUOS MINEROS (JALES OCOLAS) DE MINERALIZACIÓN DE TIPO EPITERMAL, HIDALGO, MÉXICO Raúl Moreno Geología México tailings epithermal neoformation Mining district |
| title_short |
EVALUACIÓN GEOQUÍMICA DE RESIDUOS MINEROS (JALES OCOLAS) DE MINERALIZACIÓN DE TIPO EPITERMAL, HIDALGO, MÉXICO |
| title_full |
EVALUACIÓN GEOQUÍMICA DE RESIDUOS MINEROS (JALES OCOLAS) DE MINERALIZACIÓN DE TIPO EPITERMAL, HIDALGO, MÉXICO |
| title_fullStr |
EVALUACIÓN GEOQUÍMICA DE RESIDUOS MINEROS (JALES OCOLAS) DE MINERALIZACIÓN DE TIPO EPITERMAL, HIDALGO, MÉXICO |
| title_full_unstemmed |
EVALUACIÓN GEOQUÍMICA DE RESIDUOS MINEROS (JALES OCOLAS) DE MINERALIZACIÓN DE TIPO EPITERMAL, HIDALGO, MÉXICO |
| title_sort |
EVALUACIÓN GEOQUÍMICA DE RESIDUOS MINEROS (JALES OCOLAS) DE MINERALIZACIÓN DE TIPO EPITERMAL, HIDALGO, MÉXICO |
| dc.creator.none.fl_str_mv |
Raúl Moreno Marcos G. Monroy E. Pedro Castañeda |
| author |
Raúl Moreno |
| author_facet |
Raúl Moreno Marcos G. Monroy E. Pedro Castañeda |
| author_role |
author |
| author2 |
Marcos G. Monroy E. Pedro Castañeda |
| author2_role |
author author |
| dc.subject.none.fl_str_mv |
Geología México tailings epithermal neoformation Mining district |
| topic |
Geología México tailings epithermal neoformation Mining district |
| description |
He mining district Pachuca-Real del Monte is located to the center-east of Mexico, between the geographical coordinates 20°07’30” of north latitude and 98°44 ‘00 “ of length west. The residues are derived from an epithermal mineralization. Concentrations of Pb and the Mn are significant. The mineralization consists of pyrite, limonite-goethite-hematite, sphalerite, galena, and chalcopyrite associated with quartz, calcite and silicates. X-rays diffraction patterns determined quartz as the mayor mineral phase, with minor gypsum, calcite, alunite, and pyrite. The statistical analysis showed the frequent association of Zn-Cd. The microanalysis with the scanning electronic microscope and electronic microprobe showed the neoformation of the pyrite and the oxidation and precipitate of sulfides. The tests NOM-053 and EPA-1312 showed that the Cd, Ni, Ag, Pb Mn, Zn, and As do not exceed the LMP. Only the Pb is superior to the LMP in the first test. These residues might be classified as dangerous with regard to the Pb. |
| publishDate |
2009 |
| dc.date.none.fl_str_mv |
2009 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/article |
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article |
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publishedVersion |
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0256-7024 https://www.redalyc.org/articulo.oa?id=45437348007 |
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0256-7024 |
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https://www.redalyc.org/articulo.oa?id=45437348007 |
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es |
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es |
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http://www.redalyc.org/revista.oa?id=454 |
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Revista Geológica de América Central info:eu-repo/semantics/openAccess |
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Revista Geológica de América Central |
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openAccess |
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application/pdf |
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Universidad de Costa Rica |
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Universidad de Costa Rica |
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Revista Geológica de América Central (Costa Rica) Num.41 reponame:Redalyc-UASLP instname:Universidad Autónoma de San Luis Potosí instacron:UASLP |
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Universidad Autónoma de San Luis Potosí |
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UASLP |
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