Paleogeographic boundary in the evolution of the Pucara Basin (Triassic-Liassic) and the Arequipa basin (Lias-Dogger): an inheritance of the block accreted during the Mesoproterozoic

Descripción del Articulo

páginas 50-52.
Detalles Bibliográficos
Autores: Carlotto Caillaux, Víctor Santiago, Cárdenas Roque, José Dionicio, Cano Lazo, Vilma Antonia, Rodríguez Mejía, Rildo
Formato: objeto de conferencia
Fecha de Publicación:2009
Institución:Instituto Geológico, Minero y Metalúrgico
Repositorio:INGEMMET-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.ingemmet.gob.pe:20.500.12544/1920
Enlace del recurso:https://hdl.handle.net/20.500.12544/1920
Nivel de acceso:acceso abierto
Materia:Paleogeografía
Deformación
Paleoambientes
Sedimentación
Subducción
Tectónica
Paleogeographic
Cuenca Arequipa
Cuenca Pucará
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dc.title.es_PE.fl_str_mv Paleogeographic boundary in the evolution of the Pucara Basin (Triassic-Liassic) and the Arequipa basin (Lias-Dogger): an inheritance of the block accreted during the Mesoproterozoic
title Paleogeographic boundary in the evolution of the Pucara Basin (Triassic-Liassic) and the Arequipa basin (Lias-Dogger): an inheritance of the block accreted during the Mesoproterozoic
spellingShingle Paleogeographic boundary in the evolution of the Pucara Basin (Triassic-Liassic) and the Arequipa basin (Lias-Dogger): an inheritance of the block accreted during the Mesoproterozoic
Carlotto Caillaux, Víctor Santiago
Paleogeografía
Deformación
Paleoambientes
Sedimentación
Subducción
Tectónica
Paleogeographic
Cuenca Arequipa
Cuenca Pucará
title_short Paleogeographic boundary in the evolution of the Pucara Basin (Triassic-Liassic) and the Arequipa basin (Lias-Dogger): an inheritance of the block accreted during the Mesoproterozoic
title_full Paleogeographic boundary in the evolution of the Pucara Basin (Triassic-Liassic) and the Arequipa basin (Lias-Dogger): an inheritance of the block accreted during the Mesoproterozoic
title_fullStr Paleogeographic boundary in the evolution of the Pucara Basin (Triassic-Liassic) and the Arequipa basin (Lias-Dogger): an inheritance of the block accreted during the Mesoproterozoic
title_full_unstemmed Paleogeographic boundary in the evolution of the Pucara Basin (Triassic-Liassic) and the Arequipa basin (Lias-Dogger): an inheritance of the block accreted during the Mesoproterozoic
title_sort Paleogeographic boundary in the evolution of the Pucara Basin (Triassic-Liassic) and the Arequipa basin (Lias-Dogger): an inheritance of the block accreted during the Mesoproterozoic
author Carlotto Caillaux, Víctor Santiago
author_facet Carlotto Caillaux, Víctor Santiago
Cárdenas Roque, José Dionicio
Cano Lazo, Vilma Antonia
Rodríguez Mejía, Rildo
author_role author
author2 Cárdenas Roque, José Dionicio
Cano Lazo, Vilma Antonia
Rodríguez Mejía, Rildo
author2_role author
author
author
dc.contributor.author.fl_str_mv Carlotto Caillaux, Víctor Santiago
Cárdenas Roque, José Dionicio
Cano Lazo, Vilma Antonia
Rodríguez Mejía, Rildo
dc.subject.es_PE.fl_str_mv Paleogeografía
Deformación
Paleoambientes
Sedimentación
Subducción
Tectónica
Paleogeographic
Cuenca Arequipa
Cuenca Pucará
topic Paleogeografía
Deformación
Paleoambientes
Sedimentación
Subducción
Tectónica
Paleogeographic
Cuenca Arequipa
Cuenca Pucará
description páginas 50-52.
publishDate 2009
dc.date.accessioned.none.fl_str_mv 2019-01-15T23:02:18Z
dc.date.available.none.fl_str_mv 2019-01-15T23:02:18Z
dc.date.issued.fl_str_mv 2009
dc.type.es_PE.fl_str_mv info:eu-repo/semantics/conferenceObject
format conferenceObject
dc.identifier.isbn.none.fl_str_mv urn:isbn:9783940344779
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12544/1920
dc.identifier.bibliographicCitation.es_PE.fl_str_mv International Lateinamerika-Kolloquium 2009 : abstracts and program, 2009
identifier_str_mv urn:isbn:9783940344779
International Lateinamerika-Kolloquium 2009 : abstracts and program, 2009
url https://hdl.handle.net/20.500.12544/1920
dc.language.iso.es_PE.fl_str_mv eng
language eng
dc.rights.es_PE.fl_str_mv info:eu-repo/semantics/openAccess
dc.rights.uri.es_PE.fl_str_mv http://creativecommons.org/licenses/by-nd/2.0/de/deed.en
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by-nd/2.0/de/deed.en
dc.format.es_PE.fl_str_mv application/pdf
dc.coverage.spatial.es_PE.fl_str_mv Arequipa
Cusco
Puno
Perú
dc.coverage.temporal.none.fl_str_mv Mesoproterozoico
dc.publisher.es_PE.fl_str_mv Universitätsverlag Göttingen
dc.publisher.country.es_PE.fl_str_mv DE
dc.source.es_PE.fl_str_mv Instituto Geológico, Minero y Metalúrgico – INGEMMET
Repositorio Institucional INGEMMET
dc.source.none.fl_str_mv reponame:INGEMMET-Institucional
instname:Instituto Geológico, Minero y Metalúrgico
instacron:INGEMMET
instname_str Instituto Geológico, Minero y Metalúrgico
instacron_str INGEMMET
institution INGEMMET
reponame_str INGEMMET-Institucional
collection INGEMMET-Institucional
bitstream.url.fl_str_mv https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/1920/1/Carlotto-Paleogeographic_boundary_in_the_evolution.pdf
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spelling Carlotto Caillaux, Víctor SantiagoCárdenas Roque, José DionicioCano Lazo, Vilma AntoniaRodríguez Mejía, RildoArequipaCuscoPunoPerúMesoproterozoico2019-01-15T23:02:18Z2019-01-15T23:02:18Z2009urn:isbn:9783940344779https://hdl.handle.net/20.500.12544/1920International Lateinamerika-Kolloquium 2009 : abstracts and program, 2009páginas 50-52.Summarizing, the older Cusco-Puno High has a deeper metasomized lerzholithic mantle lithosphere below the Western Altiplano. This block is separated from the Western Cordillera by the C-L-M fault system. Beneath the Eastern Altiplano, corresponds to a Paleoproterozoic to Archaic metasomatized harzburgite mantle. This is added to the presence of the Arequipa Massif (with ages between 1900 and 600 Ma) which is the basement of the Western Cordillera (oldest Arequipa basin). Hence, the lithosphere of the western margin of the South American continent is a mosaic of amalgamated lithospheric blocks (terranes) accreted to Amazonia during the Sunsás orogeny at 1000 Ma. This was a complex collision between a large block, the Arequipa Massif, and other small lithospheric blocks which later formed the substrate for the Western and Eastern Altiplano. If we consider the Totos-Paras High as a prolongation of the Cusco-Puno High, then the substrate would be the same which comes from Cusco-Puno High. This study shows how the older structures control not only Meso-Cenozoic paleogeography, but also Andean deformation.application/pdfengUniversitätsverlag GöttingenDEinfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nd/2.0/de/deed.enInstituto Geológico, Minero y Metalúrgico – INGEMMETRepositorio Institucional INGEMMETreponame:INGEMMET-Institucionalinstname:Instituto Geológico, Minero y Metalúrgicoinstacron:INGEMMETPaleogeografíaDeformaciónPaleoambientesSedimentaciónSubducciónTectónicaPaleogeographicCuenca ArequipaCuenca PucaráPaleogeographic boundary in the evolution of the Pucara Basin (Triassic-Liassic) and the Arequipa basin (Lias-Dogger): an inheritance of the block accreted during the Mesoproterozoicinfo:eu-repo/semantics/conferenceObjectPaleontologíaORIGINALCarlotto-Paleogeographic_boundary_in_the_evolution.pdfCarlotto-Paleogeographic_boundary_in_the_evolution.pdfArtículo de congresoapplication/pdf139374https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/1920/1/Carlotto-Paleogeographic_boundary_in_the_evolution.pdfad8dd27d50031e118a922a463c3a7a6fMD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81567https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/1920/2/license.txtecccc10c448afdeacc04912e07a3ed65MD52TEXTCarlotto-Paleogeographic_boundary_in_the_evolution.pdf.txtCarlotto-Paleogeographic_boundary_in_the_evolution.pdf.txtExtracted texttext/plain9775https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/1920/3/Carlotto-Paleogeographic_boundary_in_the_evolution.pdf.txtafedba5b6dee1c7687f76bc998895e69MD53THUMBNAILCarlotto-Paleogeographic_boundary_in_the_evolution.pdf.jpgCarlotto-Paleogeographic_boundary_in_the_evolution.pdf.jpgGenerated Thumbnailimage/jpeg22649https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/1920/4/Carlotto-Paleogeographic_boundary_in_the_evolution.pdf.jpg927d19681cdb0aee97ed32d993eed607MD5420.500.12544/1920oai:repositorio.ingemmet.gob.pe:20.500.12544/19202019-01-16 03:01:05.525Repositorio Institucional INGEMMETrepositorio@ingemmet.gob.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Paleogeographic boundary in the evolution of the Pucara Basin (Triassic-Liassic) and the Arequipa basin (Lias-Dogger): an inheritance of the block accreted during the Mesoproterozoic
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