Lead-zinc deposits of Cordillera Blanca and northern Cordillera Huayhuash, Peru

Descripción del Articulo

166 páginas, 12 láminas | Elaborado en cooperación con el Ministerio de Fomento, Instituto Geológico del Perú, bajo el auspicio del Interdepartmental Committee on Scientific and Cultural Cooperation Department of State (U.S.).
Detalles Bibliográficos
Autores: Bodenlos, Alfred J., Ericksen, George Edward
Formato: informe técnico
Fecha de Publicación:1955
Institución:Instituto Geológico, Minero y Metalúrgico
Repositorio:INGEMMET-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.ingemmet.gob.pe:20.500.12544/2439
Enlace del recurso:https://hdl.handle.net/20.500.12544/2439
https://doi.org/10.3133/b1017
Nivel de acceso:acceso abierto
Materia:Geología económica
Yacimientos minerales
Plomo
Zinc
Ore deposits
Economic geology
Lead
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dc.title.es_PE.fl_str_mv Lead-zinc deposits of Cordillera Blanca and northern Cordillera Huayhuash, Peru
dc.title.alternative.es_PE.fl_str_mv Geologic investigations in American Republics
title Lead-zinc deposits of Cordillera Blanca and northern Cordillera Huayhuash, Peru
spellingShingle Lead-zinc deposits of Cordillera Blanca and northern Cordillera Huayhuash, Peru
Bodenlos, Alfred J.
Geología económica
Yacimientos minerales
Plomo
Zinc
Ore deposits
Economic geology
Lead
title_short Lead-zinc deposits of Cordillera Blanca and northern Cordillera Huayhuash, Peru
title_full Lead-zinc deposits of Cordillera Blanca and northern Cordillera Huayhuash, Peru
title_fullStr Lead-zinc deposits of Cordillera Blanca and northern Cordillera Huayhuash, Peru
title_full_unstemmed Lead-zinc deposits of Cordillera Blanca and northern Cordillera Huayhuash, Peru
title_sort Lead-zinc deposits of Cordillera Blanca and northern Cordillera Huayhuash, Peru
author Bodenlos, Alfred J.
author_facet Bodenlos, Alfred J.
Ericksen, George Edward
author_role author
author2 Ericksen, George Edward
author2_role author
dc.contributor.author.fl_str_mv Bodenlos, Alfred J.
Ericksen, George Edward
dc.subject.es_PE.fl_str_mv Geología económica
Yacimientos minerales
Plomo
Zinc
Ore deposits
Economic geology
Lead
topic Geología económica
Yacimientos minerales
Plomo
Zinc
Ore deposits
Economic geology
Lead
description 166 páginas, 12 láminas | Elaborado en cooperación con el Ministerio de Fomento, Instituto Geológico del Perú, bajo el auspicio del Interdepartmental Committee on Scientific and Cultural Cooperation Department of State (U.S.).
publishDate 1955
dc.date.accessioned.none.fl_str_mv 2019-12-23T21:48:43Z
dc.date.available.none.fl_str_mv 2019-12-23T21:48:43Z
dc.date.issued.fl_str_mv 1955
dc.type.es_PE.fl_str_mv info:eu-repo/semantics/report
format report
dc.identifier.citation.es_PE.fl_str_mv Bodenlos, A. J. & Ericksen, G. E. (1955). Lead-zinc deposits of Cordillera Blanca and northern Cordillera Huayhuash, Peru. U.S. Geological Survey Bulletin, 1017. 166 p., 12 láminas.
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12544/2439
dc.identifier.doi.none.fl_str_mv https://doi.org/10.3133/b1017
identifier_str_mv Bodenlos, A. J. & Ericksen, G. E. (1955). Lead-zinc deposits of Cordillera Blanca and northern Cordillera Huayhuash, Peru. U.S. Geological Survey Bulletin, 1017. 166 p., 12 láminas.
url https://hdl.handle.net/20.500.12544/2439
https://doi.org/10.3133/b1017
dc.language.iso.es_PE.fl_str_mv eng
language eng
dc.relation.ispartofseries.none.fl_str_mv U.S. Geological Survey Bulletin;n° 1017
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dc.format.es_PE.fl_str_mv application/pdf
dc.coverage.spatial.es_PE.fl_str_mv Cordillera Blanca
Cordillera de Huayhuash
Ancash
Perú
dc.publisher.es_PE.fl_str_mv United States Government Printing Office
dc.publisher.country.es_PE.fl_str_mv US
dc.source.es_PE.fl_str_mv Instituto Geológico, Minero y Metalúrgico – INGEMMET
Repositorio Institucional INGEMMET
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spelling Bodenlos, Alfred J.Ericksen, George EdwardCordillera BlancaCordillera de HuayhuashAncashPerú2019-12-23T21:48:43Z2019-12-23T21:48:43Z1955Bodenlos, A. J. & Ericksen, G. E. (1955). Lead-zinc deposits of Cordillera Blanca and northern Cordillera Huayhuash, Peru. U.S. Geological Survey Bulletin, 1017. 166 p., 12 láminas.https://hdl.handle.net/20.500.12544/2439https://doi.org/10.3133/b1017166 páginas, 12 láminas | Elaborado en cooperación con el Ministerio de Fomento, Instituto Geológico del Perú, bajo el auspicio del Interdepartmental Committee on Scientific and Cultural Cooperation Department of State (U.S.).Base metal deposits in the central and southern Cordillera Blanca and the northern Cordillera Huayhuash comprise 6 mineral districts, 5 in the Departamento cle Ancash and 1 in the neighboring Departamento de Huanuco. Although many of the deposits were prospected and some mined on a small scale during the Spanish Colonial period, most activity has taken place in the last hundred years. Concentrates were produced in 194S and 1949 at the rate of about 1,000 tons annually, and the rate of production during ceveral previous years was evidently about the same. Silver-bearing galena concentrate is the chief product. Sphalerite either is not mined or is discarded because its value lias been too low to cover costs of production and transportation. The sedimentary rock units of the region are Jurassic (?) marine quartzites and phyllites, Lower Neocomian iluviatile and brackish-water sandstones, shales, and coals, Barremian marine and nonmarine limestones, marls, shales, and tuffs, and Middle Cretaceous marine limestones. During a period of orogeny beginning at the end of the Cretaceous the sedimentary sequence was compressed, commonly forming upright folds, but also some recumbent folds, many small bedding-plane faults, and some large reverse faults. At or near the end of deformation the sedimentary rocks were intruded by a batholith of granodiorite. The sedimentary rocks are slightly metamorphosed on a regional scale as a result of folding and locally are more highly metamorphosed in zones bordering igneous bodies. During subsequent uplift of the Andean block the sedimentary rocks were dislocated along normal faults and intruded by igneous stocks, dikes, and sills. Deposition of base metals is thought to have accompanied or immediately followed this stage of igneous activity. The most common sulflde minerals in the deposits are galena, sphalerite, and pyrite; chalcopyrite, tetrahedrite-teunantite, arsenopyrite, and stibuite may also be present. Silver occurs in galena, in the copper sulfides, or as free sulfides. The sulflde minerals are oxidized to shallow depths, and the upper parts of many veins have been secondarily enriched in silver. Common non-metallic gangue minerals in most deposits are quartz and carbonates; fluorite and barite are found in some deposits, and silicate minerals are found in contact deposits in calcareous rocks. Most deposits are fissure filling veins along small fault or shear zones, but a number are replacements of wall rock along small faults, certain sedimentary beds, or contact zones. The fissure filling veins occur in any type of country rock, sedimentary, metaseclimentary, or igneous. Most replacement deposits are in calcareous rocks, but a few are in other rock types. Mineralogy and textures of the deposits indicate that nearly all are within the range of inesotherrual-epithermal origin.Mineralized faults and shear zones are from several hundred meters to more than a kilometer long and have vertical extents of at most a few hundred meters; they are generally from 0.0 to 1 meter wide. Ore shoots containing argentiferous galena occupy only a fraction of such structures, have sporadic distribution, and in most deposits are small and lenticular, with galena ranging in tenor from 5 to SO percent. Replacement deposits have a wide range in size and are characterized by a low tenor of galena. At most mines ore is mined selectively, crushed, and concentrated by hand. For this reason fissure-filling veins containing ore shoots with high tenor of galena are preferred by miners. Small concentrators in the Quebrada Honda-Vesuvio and the Pachapaqui districts treat ore from only a few deposits. The size of ore bodies in most deposits precludes larger scale mining or mechanizations of operations, and it is concluded that only minor expansion of production is possible under existing conditions. The greatest deterrent to increased production is the high cost of transportation of concentrates by pack animals to roadheads. It is recommended that access roads be constructed to, or at least part way to, four of the mineral districts. With reduced transportation costs, miners could extract lower grade ore. Construction of small mills in other districts would also permit mining of lower grade ore. Replacement deposits of lead-zinc sulfides in the Pacllon-Llamac and Pachapaqui districts and copper sulfldes in the Antamina-Contonga district contain large reserves of possibly minable material. However, development of these deposits would require large investments in roads, concentrating plants, and mining machinery.application/pdfengUnited States Government Printing OfficeUSU.S. Geological Survey Bulletin;n° 1017info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/4.0/deed.esInstituto Geológico, Minero y Metalúrgico – INGEMMETRepositorio Institucional INGEMMETreponame:INGEMMET-Institucionalinstname:Instituto Geológico, Minero y Metalúrgicoinstacron:INGEMMETGeología económicaYacimientos mineralesPlomoZincOre depositsEconomic geologyLeadLead-zinc deposits of Cordillera Blanca and northern Cordillera Huayhuash, PeruGeologic investigations in American 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texttext/plain1https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/53/Bodenlos-plate-07.pdf.txt68b329da9893e34099c7d8ad5cb9c940MD553Bodenlos-plate-08.pdf.txtBodenlos-plate-08.pdf.txtExtracted texttext/plain1https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/55/Bodenlos-plate-08.pdf.txt68b329da9893e34099c7d8ad5cb9c940MD555Bodenlos-plate-09.pdf.txtBodenlos-plate-09.pdf.txtExtracted texttext/plain1https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/57/Bodenlos-plate-09.pdf.txt68b329da9893e34099c7d8ad5cb9c940MD557Bodenlos-plate-10.pdf.txtBodenlos-plate-10.pdf.txtExtracted texttext/plain1https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/59/Bodenlos-plate-10.pdf.txt68b329da9893e34099c7d8ad5cb9c940MD559Bodenlos-plate-11.pdf.txtBodenlos-plate-11.pdf.txtExtracted texttext/plain1https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/61/Bodenlos-plate-11.pdf.txt68b329da9893e34099c7d8ad5cb9c940MD561Bodenlos-plate-12.pdf.txtBodenlos-plate-12.pdf.txtExtracted texttext/plain1https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/63/Bodenlos-plate-12.pdf.txt68b329da9893e34099c7d8ad5cb9c940MD563THUMBNAILBodenlos-plate-01.pdf.jpgBodenlos-plate-01.pdf.jpgGenerated Thumbnailimage/jpeg20180https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/42/Bodenlos-plate-01.pdf.jpgb21a800056117ab70a53810fa84e6c4bMD542Bodenlos-plate-02.pdf.jpgBodenlos-plate-02.pdf.jpgGenerated Thumbnailimage/jpeg16400https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/44/Bodenlos-plate-02.pdf.jpg020d6825bbb5d112e470c77011deab1dMD544Bodenlos-plate-03.pdf.jpgBodenlos-plate-03.pdf.jpgGenerated Thumbnailimage/jpeg18682https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/46/Bodenlos-plate-03.pdf.jpg695fc8a7ac8392518eddf33699b2050bMD546Bodenlos-plate-04.pdf.jpgBodenlos-plate-04.pdf.jpgGenerated Thumbnailimage/jpeg14122https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/48/Bodenlos-plate-04.pdf.jpg8718fee3bd5b4ac98e9747e325a31770MD548Bodenlos-plate-05.pdf.jpgBodenlos-plate-05.pdf.jpgGenerated Thumbnailimage/jpeg17639https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/50/Bodenlos-plate-05.pdf.jpgcc59316ffaa42295ee75d5e2fdc12715MD550Bodenlos-plate-06.pdf.jpgBodenlos-plate-06.pdf.jpgGenerated Thumbnailimage/jpeg18339https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/52/Bodenlos-plate-06.pdf.jpg4abcf1e8817f4851971583ed40e86ab8MD552Bodenlos-plate-07.pdf.jpgBodenlos-plate-07.pdf.jpgGenerated Thumbnailimage/jpeg11972https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/54/Bodenlos-plate-07.pdf.jpg507d6877d7c9edafdf0bea90a9d202deMD554Bodenlos-plate-08.pdf.jpgBodenlos-plate-08.pdf.jpgGenerated Thumbnailimage/jpeg9198https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/56/Bodenlos-plate-08.pdf.jpga5227c1e4e68bad0ccb29eb864ac2ab1MD556Bodenlos-plate-09.pdf.jpgBodenlos-plate-09.pdf.jpgGenerated Thumbnailimage/jpeg18591https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/58/Bodenlos-plate-09.pdf.jpg1afb010cd0c8e8e3de7596458fa71f8eMD558Bodenlos-plate-10.pdf.jpgBodenlos-plate-10.pdf.jpgGenerated Thumbnailimage/jpeg12247https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/60/Bodenlos-plate-10.pdf.jpgd9e5f2519c9e450e50a0e0807f9a9769MD560Bodenlos-plate-11.pdf.jpgBodenlos-plate-11.pdf.jpgGenerated Thumbnailimage/jpeg19275https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/62/Bodenlos-plate-11.pdf.jpg27c304230c9dece1d83bd739f59dc821MD562Bodenlos-plate-12.pdf.jpgBodenlos-plate-12.pdf.jpgGenerated Thumbnailimage/jpeg20958https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/64/Bodenlos-plate-12.pdf.jpg9ce20af4bf62eaa290e69e4476264cd4MD564Bodenlos-Lead-zinc_deposits_Cordillera_Blanca.pdf.jpgBodenlos-Lead-zinc_deposits_Cordillera_Blanca.pdf.jpgGenerated Thumbnailimage/jpeg19382https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/66/Bodenlos-Lead-zinc_deposits_Cordillera_Blanca.pdf.jpgaa4576f7aeafe4c0a2ac003153ad0ad7MD566portada 2439.jpg.jpgportada 2439.jpg.jpgGenerated Thumbnailimage/jpeg19382https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2439/67/portada%202439.jpg.jpgaa4576f7aeafe4c0a2ac003153ad0ad7MD56720.500.12544/2439oai:repositorio.ingemmet.gob.pe:20.500.12544/24392023-04-17 14:34:42.651Repositorio Institucional INGEMMETrepositorio@ingemmet.gob.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
score 13.889614
Lead-zinc deposits of Cordillera Blanca and northern Cordillera Huayhuash, Peru
Nota importante:
La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).

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