Preparation of the Log type of rock - log integration and Sequential Stratigraphy methodology in the complex reservoirs of the units, Tarma-Copacabana system in Madre de Dios Basin
Descripción del Articulo
Carbonaceous rocks in Peru have been little studied because of the mineralogical variability, their poorly understood sedimentation processes and the complexity of their rock attributes (porosity, permeability). The objective of the present research is to obtain an integrated log type that serves as...
| Autor: | |
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| Formato: | artículo |
| Fecha de Publicación: | 2019 |
| Institución: | Universidad Nacional Mayor de San Marcos |
| Repositorio: | Revistas - Universidad Nacional Mayor de San Marcos |
| Lenguaje: | español |
| OAI Identifier: | oai:ojs.csi.unmsm:article/16681 |
| Enlace del recurso: | https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/16681 |
| Nivel de acceso: | acceso abierto |
| Materia: | Deposition model; rock attributes; chained systems Modelo deposicional; atributos de roca; sistemas encadenados |
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Preparation of the Log type of rock - log integration and Sequential Stratigraphy methodology in the complex reservoirs of the units, Tarma-Copacabana system in Madre de Dios BasinElaboración del Perfil Tipo a partir de la integración Roca – Perfil y la metodología de Estratigrafía Secuencial en los reservorios complejos de las unidades sistema Tarma- Copacabana en la Cuenca Madre de DiosCastillo Guzmán, EdsonDeposition model; rock attributes; chained systemsModelo deposicional; atributos de roca; sistemas encadenadosCarbonaceous rocks in Peru have been little studied because of the mineralogical variability, their poorly understood sedimentation processes and the complexity of their rock attributes (porosity, permeability). The objective of the present research is to obtain an integrated log type that serves as a standard for the elaboration of geological sections and maps, in order to establish a predictive model, in an areal distribution of potential reservoirs within calcareous units. Tarma and Copacabana groups mainly composed of carbonaceous facies, with a lower proportion of silicoclastics and evaporites, all have thicknesses ranging from 800 to 1000 meters. Within the depositional model, 4 sequences have been identified in the third order, from Continental Environments to Distal marine. It is seen that within each sequence of third order have been related up to three sedimentary courts; (Continental), transgressive and high seas (platform), which integrates them with the attributes of rock, it is identified that the levels of porosity are found in the LST and HST systems.Las rocas carbonáticas en el Perú han sido poco estudiadas, debido a su variabilidad mineralógica, a sus procesos de sedimentación poco entendidos y a la complejidad de sus atributos de roca (porosidad, permeabilidad). El objetivo de la presente investigación es obtener el perfil tipo integrado que sirva de patrón de correlación para la interpretación de las secciones geológicas y mapas, con el fin de elaborar un modelo predictivo, con la distribución areal de potenciales reservorios dentro de los Grupos Tarma y Copacabana compuestos principalmente de facies carbonáticas y en menor proporción silicoclásticas y evaporíticas en conjunto tienen espesores que van desde los 800 m a 1000 m. El modelo deposicional – genético ha identificado 4 secuencias en tercer orden, que encadenan ambientes desde continentales hasta marinos distales. Se aprecia que dentro de cada secuencia se han relacionado hasta tres cortejos sedimentarios: sistema de mar bajo (continental), sistema transgresivo y sistema de mar alto (plataforma interna – externa y marino), que definen los atributos de roca identificándose los niveles con porosidad dentro de los sistemas de mar bajo (LST) y alto (HST).Universidad Nacional Mayor de San Marcos, Facultad de Ingeniería Geológica, Minera, Metalúrgica y Geográfica2019-07-15info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/1668110.15381/iigeo.v22i43.16681Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 22 No. 43 (2019); 9-20Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 22 Núm. 43 (2019); 9-201682-30871561-0888reponame:Revistas - Universidad Nacional Mayor de San Marcosinstname:Universidad Nacional Mayor de San Marcosinstacron:UNMSMspahttps://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/16681/14247Derechos de autor 2019 Edson J. Castillo Guzmánhttps://creativecommons.org/licenses/by-nc-sa/4.0info:eu-repo/semantics/openAccessoai:ojs.csi.unmsm:article/166812020-03-11T22:21:30Z |
| dc.title.none.fl_str_mv |
Preparation of the Log type of rock - log integration and Sequential Stratigraphy methodology in the complex reservoirs of the units, Tarma-Copacabana system in Madre de Dios Basin Elaboración del Perfil Tipo a partir de la integración Roca – Perfil y la metodología de Estratigrafía Secuencial en los reservorios complejos de las unidades sistema Tarma- Copacabana en la Cuenca Madre de Dios |
| title |
Preparation of the Log type of rock - log integration and Sequential Stratigraphy methodology in the complex reservoirs of the units, Tarma-Copacabana system in Madre de Dios Basin |
| spellingShingle |
Preparation of the Log type of rock - log integration and Sequential Stratigraphy methodology in the complex reservoirs of the units, Tarma-Copacabana system in Madre de Dios Basin Castillo Guzmán, Edson Deposition model; rock attributes; chained systems Modelo deposicional; atributos de roca; sistemas encadenados |
| title_short |
Preparation of the Log type of rock - log integration and Sequential Stratigraphy methodology in the complex reservoirs of the units, Tarma-Copacabana system in Madre de Dios Basin |
| title_full |
Preparation of the Log type of rock - log integration and Sequential Stratigraphy methodology in the complex reservoirs of the units, Tarma-Copacabana system in Madre de Dios Basin |
| title_fullStr |
Preparation of the Log type of rock - log integration and Sequential Stratigraphy methodology in the complex reservoirs of the units, Tarma-Copacabana system in Madre de Dios Basin |
| title_full_unstemmed |
Preparation of the Log type of rock - log integration and Sequential Stratigraphy methodology in the complex reservoirs of the units, Tarma-Copacabana system in Madre de Dios Basin |
| title_sort |
Preparation of the Log type of rock - log integration and Sequential Stratigraphy methodology in the complex reservoirs of the units, Tarma-Copacabana system in Madre de Dios Basin |
| dc.creator.none.fl_str_mv |
Castillo Guzmán, Edson |
| author |
Castillo Guzmán, Edson |
| author_facet |
Castillo Guzmán, Edson |
| author_role |
author |
| dc.subject.none.fl_str_mv |
Deposition model; rock attributes; chained systems Modelo deposicional; atributos de roca; sistemas encadenados |
| topic |
Deposition model; rock attributes; chained systems Modelo deposicional; atributos de roca; sistemas encadenados |
| description |
Carbonaceous rocks in Peru have been little studied because of the mineralogical variability, their poorly understood sedimentation processes and the complexity of their rock attributes (porosity, permeability). The objective of the present research is to obtain an integrated log type that serves as a standard for the elaboration of geological sections and maps, in order to establish a predictive model, in an areal distribution of potential reservoirs within calcareous units. Tarma and Copacabana groups mainly composed of carbonaceous facies, with a lower proportion of silicoclastics and evaporites, all have thicknesses ranging from 800 to 1000 meters. Within the depositional model, 4 sequences have been identified in the third order, from Continental Environments to Distal marine. It is seen that within each sequence of third order have been related up to three sedimentary courts; (Continental), transgressive and high seas (platform), which integrates them with the attributes of rock, it is identified that the levels of porosity are found in the LST and HST systems. |
| publishDate |
2019 |
| dc.date.none.fl_str_mv |
2019-07-15 |
| 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/16681 10.15381/iigeo.v22i43.16681 |
| url |
https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/16681 |
| identifier_str_mv |
10.15381/iigeo.v22i43.16681 |
| 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/16681/14247 |
| dc.rights.none.fl_str_mv |
Derechos de autor 2019 Edson J. Castillo Guzmán https://creativecommons.org/licenses/by-nc-sa/4.0 info:eu-repo/semantics/openAccess |
| rights_invalid_str_mv |
Derechos de autor 2019 Edson J. Castillo Guzmán 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. 22 No. 43 (2019); 9-20 Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 22 Núm. 43 (2019); 9-20 1682-3087 1561-0888 reponame:Revistas - Universidad Nacional Mayor de San Marcos instname:Universidad Nacional Mayor de San Marcos instacron:UNMSM |
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Universidad Nacional Mayor de San Marcos |
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UNMSM |
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UNMSM |
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Revistas - Universidad Nacional Mayor de San Marcos |
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Revistas - Universidad Nacional Mayor de San Marcos |
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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).
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).