Emerging basins, hydrocarbon potential of the Jurassic and Paleozoic carbonate reservoirs in the peruvian sub-andean belt

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The carbonate rocks in the world produce about 60% of the world consumption of hydrocarbons, the largest production of these reservoirs come from the Middle East. In Peru we produce sandstones that belong to the group of clastic rocks that historically in the world were the targets that stored hydro...

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Detalles Bibliográficos
Autor: Vásquez Flores, Marco Antonio
Formato: artículo
Fecha de Publicación:2016
Institución:Universidad Nacional Mayor de San Marcos
Repositorio:Revistas - Universidad Nacional Mayor de San Marcos
Lenguaje:español
OAI Identifier:oai:ojs.csi.unmsm:article/12963
Enlace del recurso:https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/12963
Nivel de acceso:acceso abierto
Materia:Carbonates
Tarma Group
Copacabana Group
Paleozoic
Jurassic
deposit environment
petrophysics
geophysics
Carbonatos
Grupo Tarma
Grupo Copacabana
Grupo Pucara
paleozoico
jurásico
ambiente de depósito
petrofísica
geofísica.
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oai_identifier_str oai:ojs.csi.unmsm:article/12963
network_acronym_str REVUNMSM
network_name_str Revistas - Universidad Nacional Mayor de San Marcos
repository_id_str
dc.title.none.fl_str_mv Emerging basins, hydrocarbon potential of the Jurassic and Paleozoic carbonate reservoirs in the peruvian sub-andean belt
Cuencas emergentes, potencial hidrocarburífero de los reservorios carbonatados del Jurásico y Paleozoico en la faja subandina peruana
title Emerging basins, hydrocarbon potential of the Jurassic and Paleozoic carbonate reservoirs in the peruvian sub-andean belt
spellingShingle Emerging basins, hydrocarbon potential of the Jurassic and Paleozoic carbonate reservoirs in the peruvian sub-andean belt
Vásquez Flores, Marco Antonio
Carbonates
Tarma Group
Copacabana Group
Paleozoic
Jurassic
deposit environment
petrophysics
geophysics
Carbonatos
Grupo Tarma
Grupo Copacabana
Grupo Pucara
paleozoico
jurásico
ambiente de depósito
petrofísica
geofísica.
title_short Emerging basins, hydrocarbon potential of the Jurassic and Paleozoic carbonate reservoirs in the peruvian sub-andean belt
title_full Emerging basins, hydrocarbon potential of the Jurassic and Paleozoic carbonate reservoirs in the peruvian sub-andean belt
title_fullStr Emerging basins, hydrocarbon potential of the Jurassic and Paleozoic carbonate reservoirs in the peruvian sub-andean belt
title_full_unstemmed Emerging basins, hydrocarbon potential of the Jurassic and Paleozoic carbonate reservoirs in the peruvian sub-andean belt
title_sort Emerging basins, hydrocarbon potential of the Jurassic and Paleozoic carbonate reservoirs in the peruvian sub-andean belt
dc.creator.none.fl_str_mv Vásquez Flores, Marco Antonio
author Vásquez Flores, Marco Antonio
author_facet Vásquez Flores, Marco Antonio
author_role author
dc.subject.none.fl_str_mv Carbonates
Tarma Group
Copacabana Group
Paleozoic
Jurassic
deposit environment
petrophysics
geophysics
Carbonatos
Grupo Tarma
Grupo Copacabana
Grupo Pucara
paleozoico
jurásico
ambiente de depósito
petrofísica
geofísica.
topic Carbonates
Tarma Group
Copacabana Group
Paleozoic
Jurassic
deposit environment
petrophysics
geophysics
Carbonatos
Grupo Tarma
Grupo Copacabana
Grupo Pucara
paleozoico
jurásico
ambiente de depósito
petrofísica
geofísica.
description The carbonate rocks in the world produce about 60% of the world consumption of hydrocarbons, the largest production of these reservoirs come from the Middle East. In Peru we produce sandstones that belong to the group of clastic rocks that historically in the world were the targets that stored hydrocarbons. The objective of this study is to propose new reservoirs in carbonate rocks to explore for hydrocarbons in Peru, to delimit the places where the greatest thickness has been deposited and the areas within the Peruvian territory; the Copacabana and Tarma groups belonging to the Paleozoic and the Pucará group belonging to the Mesozoic are the two largest carbonate deposits with the greatest distribution in the country. The Copacabana - Tarma groups have an areal distribution that covers almost all of Peru and includes Ecuador, Brazil, Colombia, Bolivia and northern Chile, these carbonates that belong to an open sea deposit environment, fed by the Panthalassic sea which corresponds to the time when the continent was united with Africa and North America, in Peru we find it distributed along the Andean Cordillera and in the sub-Andean region throughout the jungle from Loreto to Madre de Dios, including the basins prospects for hydrocarbons from Madre de Dios and Ucayali where it is buried and could be explored. The Pucará Group has an area distribution that includes the central and northern zones of the Andean mountain range and the western part of the sub-Andean jungle of Ucayali and Loreto that includes the Ucayali and Marañón basins where it is buried and with the possibility of being explored by hydrocarbons. . These basins with potential to explore for hydrocarbons in these proposed reservoirs are new and therefore new emerging basins for Paleozoic and Jurassic hydrocarbons are considered.
publishDate 2016
dc.date.none.fl_str_mv 2016-07-15
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/12963
10.15381/iigeo.v19i37.12963
url https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/12963
identifier_str_mv 10.15381/iigeo.v19i37.12963
dc.language.none.fl_str_mv spa
language spa
dc.relation.none.fl_str_mv https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/12963/11579
dc.rights.none.fl_str_mv Derechos de autor 2016 Marco Antonio Vásquez Flores
https://creativecommons.org/licenses/by-nc-sa/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Derechos de autor 2016 Marco Antonio Vásquez Flores
https://creativecommons.org/licenses/by-nc-sa/4.0
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidad Nacional Mayor de San Marcos, Facultad de Ingeniería Geológica, Minera, Metalúrgica y Geográfica
publisher.none.fl_str_mv Universidad Nacional Mayor de San Marcos, Facultad de Ingeniería Geológica, Minera, Metalúrgica y Geográfica
dc.source.none.fl_str_mv Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 19 No. 37 (2016)
Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 19 Núm. 37 (2016)
1682-3087
1561-0888
reponame:Revistas - Universidad Nacional Mayor de San Marcos
instname:Universidad Nacional Mayor de San Marcos
instacron:UNMSM
instname_str Universidad Nacional Mayor de San Marcos
instacron_str UNMSM
institution UNMSM
reponame_str Revistas - Universidad Nacional Mayor de San Marcos
collection Revistas - Universidad Nacional Mayor de San Marcos
repository.name.fl_str_mv
repository.mail.fl_str_mv
_version_ 1795238287107948544
spelling Emerging basins, hydrocarbon potential of the Jurassic and Paleozoic carbonate reservoirs in the peruvian sub-andean beltCuencas emergentes, potencial hidrocarburífero de los reservorios carbonatados del Jurásico y Paleozoico en la faja subandina peruanaVásquez Flores, Marco AntonioCarbonatesTarma GroupCopacabana GroupPaleozoicJurassicdeposit environmentpetrophysicsgeophysicsCarbonatosGrupo TarmaGrupo CopacabanaGrupo Pucarapaleozoicojurásicoambiente de depósitopetrofísicageofísica.The carbonate rocks in the world produce about 60% of the world consumption of hydrocarbons, the largest production of these reservoirs come from the Middle East. In Peru we produce sandstones that belong to the group of clastic rocks that historically in the world were the targets that stored hydrocarbons. The objective of this study is to propose new reservoirs in carbonate rocks to explore for hydrocarbons in Peru, to delimit the places where the greatest thickness has been deposited and the areas within the Peruvian territory; the Copacabana and Tarma groups belonging to the Paleozoic and the Pucará group belonging to the Mesozoic are the two largest carbonate deposits with the greatest distribution in the country. The Copacabana - Tarma groups have an areal distribution that covers almost all of Peru and includes Ecuador, Brazil, Colombia, Bolivia and northern Chile, these carbonates that belong to an open sea deposit environment, fed by the Panthalassic sea which corresponds to the time when the continent was united with Africa and North America, in Peru we find it distributed along the Andean Cordillera and in the sub-Andean region throughout the jungle from Loreto to Madre de Dios, including the basins prospects for hydrocarbons from Madre de Dios and Ucayali where it is buried and could be explored. The Pucará Group has an area distribution that includes the central and northern zones of the Andean mountain range and the western part of the sub-Andean jungle of Ucayali and Loreto that includes the Ucayali and Marañón basins where it is buried and with the possibility of being explored by hydrocarbons. . These basins with potential to explore for hydrocarbons in these proposed reservoirs are new and therefore new emerging basins for Paleozoic and Jurassic hydrocarbons are considered.Las rocas carbonatadas en el mundo producen cerca del 60% del consumo mundial de hidrocarburos, la mayor producción de estos reservorios provienen del Medio Oriente. En el Perú producimos de areniscas que pertenecen al grupo de rocas clásticas que históricamente en el mundo fueron los objetivos que almacenaban los hidrocarburos. Este estudio tiene como objetivo proponer nuevos reservorios en rocas carbonatadas para explorar por hidrocarburos en el Perú, delimitar los lugares donde se han depositado los mayores espesores y las áreas dentro del territorio peruano; los grupos Copacabana y Tarma pertenecientes al Paleozoico y el grupo Pucará perteneciente al Mesozoico son los dos grandes depósitos de carbonatos de mayor distribución en el país. Los grupos Copacabana – Tarma tienen una distribución areal que abarca casi todo el Perú e incluye Ecuador, Brasil, Colom-bia, Bolivia y el norte de Chile, estos carbonatos que pertenecen a un ambiente de depósito de mar abierto, alimentado por el mar Panthalassico que corresponde a la época que el continente estaba unido con África y América del Norte, en el Perú lo encontramos distribuido a lo largo de la Cordillera Andina y en el subandino en toda la zona de selva desde Loreto hasta Madre de Dios, incluyendo las cuencas prospectivas por hidrocarburos de Madre de Dios y Ucayali donde se encuentra soterrado y que podría ser explorado. El Grupo Pucará tiene una distribución areal que abarca la zona central y norte de la cordillera andina y la parte occidental del subandino de la selva de Ucayali y Loreto que incluye las cuencas Ucayali y Marañón donde se encuentra soterrado y con posibilidades de ser explorado por hidrocarburos. Estas cuencas con potencial para explorar por hidrocarburos en estos reservorios propuestos son nuevos y por eso son con-siderados nuevas cuencas emergentes para hidrocarburos del Paleozoico y Jurásico.Universidad Nacional Mayor de San Marcos, Facultad de Ingeniería Geológica, Minera, Metalúrgica y Geográfica2016-07-15info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/1296310.15381/iigeo.v19i37.12963Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 19 No. 37 (2016)Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 19 Núm. 37 (2016)1682-30871561-0888reponame:Revistas - Universidad Nacional Mayor de San Marcosinstname:Universidad Nacional Mayor de San Marcosinstacron:UNMSMspahttps://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/12963/11579Derechos de autor 2016 Marco Antonio Vásquez Floreshttps://creativecommons.org/licenses/by-nc-sa/4.0info:eu-repo/semantics/openAccessoai:ojs.csi.unmsm:article/129632020-07-11T17:36:18Z
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