Metalliferous paragenesis of the San José mine, Oruro, Bolivia
The San José silver-tin deposit, Oruro, is located in the Cordillera Oriental, which contains most of the metalliferous mineralizations of Bolivia and is related to a quartz-latite dome of Miocene age. The mineral paragenesis encountered in this study is composed of cassiterite, stannite, miargyrite...
Publicado: |
2008
|
---|---|
Materias: | |
Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v25_n4_p485_Keutsch http://hdl.handle.net/20.500.12110/paper_08959811_v25_n4_p485_Keutsch |
Aporte de: |
id |
paper:paper_08959811_v25_n4_p485_Keutsch |
---|---|
record_format |
dspace |
spelling |
paper:paper_08959811_v25_n4_p485_Keutsch2023-06-08T15:48:22Z Metalliferous paragenesis of the San José mine, Oruro, Bolivia Bolivia-mineral paragenesis Oruro San José mine mineralization Miocene ore deposit paragenesis silver tin Bolivia Oruro [Bolivia] South America The San José silver-tin deposit, Oruro, is located in the Cordillera Oriental, which contains most of the metalliferous mineralizations of Bolivia and is related to a quartz-latite dome of Miocene age. The mineral paragenesis encountered in this study is composed of cassiterite, stannite, miargyrite, pyrargyrite, andorite and Bi-rich andorite, jamesonite, pavonite/benjaminite, boulangerite, owyheeite, ramdohrite and Bi-rich ramdohrite, bismuthinite, besides pyrite, chalcopyrite, Ag-rich tetrahedrite, galena and sphalerite, all of which are analyzed by electron microprobe analysis. With semi-quantitative SEM/EDS and XRD analyses, rhodostannite and kësterite/ferrokësterite were found in association with andorite, and chalcostibite was determined by XRD, in association with zinkenite, tetrahedrite and pyrite. © 2007 Elsevier Ltd. All rights reserved. 2008 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v25_n4_p485_Keutsch http://hdl.handle.net/20.500.12110/paper_08959811_v25_n4_p485_Keutsch |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
Bolivia-mineral paragenesis Oruro San José mine mineralization Miocene ore deposit paragenesis silver tin Bolivia Oruro [Bolivia] South America |
spellingShingle |
Bolivia-mineral paragenesis Oruro San José mine mineralization Miocene ore deposit paragenesis silver tin Bolivia Oruro [Bolivia] South America Metalliferous paragenesis of the San José mine, Oruro, Bolivia |
topic_facet |
Bolivia-mineral paragenesis Oruro San José mine mineralization Miocene ore deposit paragenesis silver tin Bolivia Oruro [Bolivia] South America |
description |
The San José silver-tin deposit, Oruro, is located in the Cordillera Oriental, which contains most of the metalliferous mineralizations of Bolivia and is related to a quartz-latite dome of Miocene age. The mineral paragenesis encountered in this study is composed of cassiterite, stannite, miargyrite, pyrargyrite, andorite and Bi-rich andorite, jamesonite, pavonite/benjaminite, boulangerite, owyheeite, ramdohrite and Bi-rich ramdohrite, bismuthinite, besides pyrite, chalcopyrite, Ag-rich tetrahedrite, galena and sphalerite, all of which are analyzed by electron microprobe analysis. With semi-quantitative SEM/EDS and XRD analyses, rhodostannite and kësterite/ferrokësterite were found in association with andorite, and chalcostibite was determined by XRD, in association with zinkenite, tetrahedrite and pyrite. © 2007 Elsevier Ltd. All rights reserved. |
title |
Metalliferous paragenesis of the San José mine, Oruro, Bolivia |
title_short |
Metalliferous paragenesis of the San José mine, Oruro, Bolivia |
title_full |
Metalliferous paragenesis of the San José mine, Oruro, Bolivia |
title_fullStr |
Metalliferous paragenesis of the San José mine, Oruro, Bolivia |
title_full_unstemmed |
Metalliferous paragenesis of the San José mine, Oruro, Bolivia |
title_sort |
metalliferous paragenesis of the san josé mine, oruro, bolivia |
publishDate |
2008 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v25_n4_p485_Keutsch http://hdl.handle.net/20.500.12110/paper_08959811_v25_n4_p485_Keutsch |
_version_ |
1768546121265709056 |