Geology of the Huancavelica quicksilver district, Peru

Descripción del Articulo

45 páginas, 6 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: Yates, Robert Giertz, Kent, Dean Frederick, Fernández Concha, Jaime
Formato: informe técnico
Fecha de Publicación:1951
Institución:Instituto Geológico, Minero y Metalúrgico
Repositorio:INGEMMET-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.ingemmet.gob.pe:20.500.12544/2438
Enlace del recurso:https://hdl.handle.net/20.500.12544/2438
https://doi.org/10.3133/b975A
Nivel de acceso:acceso abierto
Materia:Geología económica
Yacimientos minerales
Minas
Mercurio
Economic geology
Quicksilver
Ore deposits
Mine
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dc.title.es_PE.fl_str_mv Geology of the Huancavelica quicksilver district, Peru
dc.title.alternative.es_PE.fl_str_mv Geologic investigations in American Republics 1950-1953
title Geology of the Huancavelica quicksilver district, Peru
spellingShingle Geology of the Huancavelica quicksilver district, Peru
Yates, Robert Giertz
Geología económica
Yacimientos minerales
Minas
Mercurio
Economic geology
Quicksilver
Ore deposits
Mine
title_short Geology of the Huancavelica quicksilver district, Peru
title_full Geology of the Huancavelica quicksilver district, Peru
title_fullStr Geology of the Huancavelica quicksilver district, Peru
title_full_unstemmed Geology of the Huancavelica quicksilver district, Peru
title_sort Geology of the Huancavelica quicksilver district, Peru
author Yates, Robert Giertz
author_facet Yates, Robert Giertz
Kent, Dean Frederick
Fernández Concha, Jaime
author_role author
author2 Kent, Dean Frederick
Fernández Concha, Jaime
author2_role author
author
dc.contributor.author.fl_str_mv Yates, Robert Giertz
Kent, Dean Frederick
Fernández Concha, Jaime
dc.subject.es_PE.fl_str_mv Geología económica
Yacimientos minerales
Minas
Mercurio
Economic geology
Quicksilver
Ore deposits
Mine
topic Geología económica
Yacimientos minerales
Minas
Mercurio
Economic geology
Quicksilver
Ore deposits
Mine
description 45 páginas, 6 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 1951
dc.date.accessioned.none.fl_str_mv 2019-12-23T21:48:20Z
dc.date.available.none.fl_str_mv 2019-12-23T21:48:20Z
dc.date.issued.fl_str_mv 1951
dc.type.es_PE.fl_str_mv info:eu-repo/semantics/report
format report
dc.identifier.citation.es_PE.fl_str_mv Yates, R. G.; Kent, D. F. & Fernández, J. (1951). Geology of the Huancavelica quicksilver district, Peru. U.S. Geological Survey Bulletin, 975-A. 45 p., 5 láminas.
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12544/2438
dc.identifier.doi.none.fl_str_mv https://doi.org/10.3133/b975A
identifier_str_mv Yates, R. G.; Kent, D. F. & Fernández, J. (1951). Geology of the Huancavelica quicksilver district, Peru. U.S. Geological Survey Bulletin, 975-A. 45 p., 5 láminas.
url https://hdl.handle.net/20.500.12544/2438
https://doi.org/10.3133/b975A
dc.language.iso.es_PE.fl_str_mv eng
language eng
dc.relation.ispartofseries.none.fl_str_mv U.S. Geological Survey Bulletin;n° 975-A
dc.rights.es_PE.fl_str_mv info:eu-repo/semantics/openAccess
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eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/4.0/deed.es
dc.format.es_PE.fl_str_mv application/pdf
dc.coverage.spatial.es_PE.fl_str_mv Huancavelica
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 Yates, Robert GiertzKent, Dean FrederickFernández Concha, JaimeHuancavelicaPerú2019-12-23T21:48:20Z2019-12-23T21:48:20Z1951Yates, R. G.; Kent, D. F. & Fernández, J. (1951). Geology of the Huancavelica quicksilver district, Peru. U.S. Geological Survey Bulletin, 975-A. 45 p., 5 láminas.https://hdl.handle.net/20.500.12544/2438https://doi.org/10.3133/b975A45 páginas, 6 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.)The Huancavelica quicksilver district, the world's largest producer of quicksilver for over a century and a half, is in the Cordillera Occidental of south-central Peru. All the important mines of the district are in a north-trending belt about 1 mile (2 kilometers) wide and 5 miles (8 kilometers) long, but a few small mines and prospects are in north and south extensions of this main belt. During the Spanish colonial period the mines produced over 1,400,000 flasks of quicksilver, most of this coming from one mine, the Santa Barbara. During the last hundred years little quicksilver has been produced, and in 1946 only one small mine was actively producing. It is not likely that the district will again become an important quicksilver-mining center unless new ore bodies are discovered or unless there prove to be unexhausted ore bodies in the inaccessible caved workings of the Santa Barbara mine. The Cordillera Occidental in central Peru is composed of Paleozoic, Mesozoic, and Tertiary sedimentary and volcanic rocks that have been folded, faulted, and intruded by various kinds of igneous rocks. In the Huancavelica district Jurassic limestones, Cretaceous sandstones, limestones, shales, and volcanic rocks, and Tertiary conglomerates, tuffs, and lavas constitute the sedimentary and volcanic rocks. Intruded into these are dacites and volcanic necks filled with pyroclastic material. The dominant structural feature is a north-trending anticline, which has a synclinal core bounded by high-angle reverse faults. Faulting accompanied and followed folding, and was itself followed by igneous intrusion and extrusion. The quicksilver deposits are classified into three types: (1) deposits occurring in sandstone, (2) deposits occurring in limestone, and (3) deposits occurring in igneous rocks. Cinnabar is the principal ore mineral and occurs mainly as a filling between sand grains in the sandstone, in fractures and porous marly bedsin the limestone, and as a filling in fractures in the igneous rocks. Other sulfide minerals are pyrite, arsenopyrite, realgar, and minor amounts of galena, sphalerite, and stibnite. Nonmetallic gangue minerals include quartz, calcite, barite, and hydrocarbons, none of which are abundant. The distribution of the ore bodies was controlled by the distribution of the more permeable sedimentary strata and of fracture openings. 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Geology of the Huancavelica quicksilver district, Peru
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