dor_id: 4132682

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650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

336.#.#.b: article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

351.#.#.6: http://revistagi.geofisica.unam.mx/index.php/RGI

351.#.#.b: Geofísica Internacional

351.#.#.a: Artículos

harvesting_group: RevistasUNAM

270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

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883.#.#.1: https://www.publicaciones.unam.mx/

883.#.#.q: Dirección General de Publicaciones y Fomento Editorial

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856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/393/406

100.1.#.a: Batista Rodríguez, Jose; Blanco Moreno, Jesús; Pérez Flores, Marco; Rodríguez Infante, Alina

524.#.#.a: Batista Rodríguez, Jose, et al. (2012). Structures and petroleum prospects of the Saramaguacán basin, Cuba, from 3D inversion of gravimetric data. Geofísica Internacional; Vol. 51 Núm. 1: Enero 1, 2012; 51-61. Recuperado de https://repositorio.unam.mx/contenidos/4132682

245.1.0.a: Structures and petroleum prospects of the Saramaguacán basin, Cuba, from 3D inversion of gravimetric data

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2012

264.#.1.c: 2012-01-01

653.#.#.a: teoría inversa; anomalías gravimétricas; estructura de la Tierra; inverse theory; Gravity anomalies; Earth structure

506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC-SA 4.0 Internacional, https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/393

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/393

041.#.7.h: spa

520.3.#.a: New structural details of the Saramaguacán basin in central Cuba are presented, based on 3D inversion of gravimetric data constrained by wells and surface geology information. The basin shows complex tectonics of the overthrust process. A probable structural analysis of the basin suggests structures of ramp and shelf, as well as the location and geometry of the basin and several sub-basins. Known location and behavior of fault depth suggests some possible new or unknown faults. Geometry variation, depth and thickness were determined for different rock formations. This has great importance for the sedimentary (oil-bearing) and paleomargin (oil-source) rocks, because it is the basis for future research to select the best sites for drilling, as well as a broad estimate calculation of hydrocarbon volume that can be stored in the oil-collector rocks. Both groups of rocks are potential targets for oil prospecting. The oil-source rocks of the Cuban system were found to be around 4 km depth. They are associated with carbonated rocks of the Paleomargin. The oil-bearing rocks reache a depth of 10 km. The 3D model obtained supports the hypothesis that the ophiolites and the Cretaceous volcanic arc rocks were tectonically emplaced from south to north, on top of carbonate-terrigenous sequences from the Bahamas paleomargin. The model shows elements of the compressive tectonics that originated the Saramaguacán basin in the Mesozoic-Tertiary. It also suggests that the Saramaguacán basin presents favorable geologic conditions for oil deposits.doi: https://doi.org/10.22201/igeof.00167169p.2012.51.1.145

773.1.#.t: Geofísica Internacional; Vol. 51 Núm. 1: Enero 1, 2012; 51-61

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169

310.#.#.a: Trimestral

300.#.#.a: Páginas: 51-61

264.#.1.b: Instituto de Geofísica, UNAM

doi: https://doi.org/10.22201/igeof.00167169p.2012.51.1.145

handle: 009f450502c0d13d

harvesting_date: 2023-06-20 16:00:00.0

856.#.0.q: application/pdf

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file_modification_date: 2022-07-04 21:54:18.0

file_creator: Jose Batista Rodríguez

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245.1.0.b: Structures and petroleum prospects of the Saramaguacán basin, Cuba, from 3D inversion of gravimetric data

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Artículo

Structures and petroleum prospects of the Saramaguacán basin, Cuba, from 3D inversion of gravimetric data

Batista Rodríguez, Jose; Blanco Moreno, Jesús; Pérez Flores, Marco; Rodríguez Infante, Alina

Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Geofísica, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Batista Rodríguez, Jose, et al. (2012). Structures and petroleum prospects of the Saramaguacán basin, Cuba, from 3D inversion of gravimetric data. Geofísica Internacional; Vol. 51 Núm. 1: Enero 1, 2012; 51-61. Recuperado de https://repositorio.unam.mx/contenidos/4132682

Descripción del recurso

Autor(es)
Batista Rodríguez, Jose; Blanco Moreno, Jesús; Pérez Flores, Marco; Rodríguez Infante, Alina
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Structures and petroleum prospects of the Saramaguacán basin, Cuba, from 3D inversion of gravimetric data
Fecha
2012-01-01
Resumen
New structural details of the Saramaguacán basin in central Cuba are presented, based on 3D inversion of gravimetric data constrained by wells and surface geology information. The basin shows complex tectonics of the overthrust process. A probable structural analysis of the basin suggests structures of ramp and shelf, as well as the location and geometry of the basin and several sub-basins. Known location and behavior of fault depth suggests some possible new or unknown faults. Geometry variation, depth and thickness were determined for different rock formations. This has great importance for the sedimentary (oil-bearing) and paleomargin (oil-source) rocks, because it is the basis for future research to select the best sites for drilling, as well as a broad estimate calculation of hydrocarbon volume that can be stored in the oil-collector rocks. Both groups of rocks are potential targets for oil prospecting. The oil-source rocks of the Cuban system were found to be around 4 km depth. They are associated with carbonated rocks of the Paleomargin. The oil-bearing rocks reache a depth of 10 km. The 3D model obtained supports the hypothesis that the ophiolites and the Cretaceous volcanic arc rocks were tectonically emplaced from south to north, on top of carbonate-terrigenous sequences from the Bahamas paleomargin. The model shows elements of the compressive tectonics that originated the Saramaguacán basin in the Mesozoic-Tertiary. It also suggests that the Saramaguacán basin presents favorable geologic conditions for oil deposits.doi: https://doi.org/10.22201/igeof.00167169p.2012.51.1.145
Tema
teoría inversa; anomalías gravimétricas; estructura de la Tierra; inverse theory; Gravity anomalies; Earth structure
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces