dor_id: 4132888

506.#.#.a: Público

590.#.#.d: Los artículos enviados a la revista "Geofísica Internacional", se juzgan por medio de un proceso de revisión por pares

510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Scientific Electronic Library Online (SciELO); SCOPUS, Dialnet, Directory of Open Access Journals (DOAJ); Geobase

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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.#.#.u: https://revistas.unam.mx/catalogo/

883.#.#.a: Revistas UNAM

590.#.#.a: Coordinación de Difusión Cultural

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

850.#.#.a: Universidad Nacional Autónoma de México

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/258/247

100.1.#.a: Batista, J. A.; Blanco, J.; Pérez-flores, M. A.

524.#.#.a: Batista, J. A., et al. (2008). Geological interpretation of eastern Cuba laterites from an airborne magnetic and radioactive isotope survey. Geofísica Internacional; Vol. 47 Núm. 2: Abril 1, 2008; 99-113. Recuperado de https://repositorio.unam.mx/contenidos/4132888

245.1.0.a: Geological interpretation of eastern Cuba laterites from an airborne magnetic and radioactive isotope survey

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2008

264.#.1.c: 2008-04-01

653.#.#.a: Cortezas lateríticas; exploración de torio y uranio; Cuba; Lateritic crust; thorium and uranium exploration; coherency

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/258

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/258

041.#.7.h: spa

520.3.#.a: In eastern Cuba area several geophysical techniques have been applied to distinguish the main geological characteristics of the laterites which are of economical importance for the extraction of iron, nickel and chrome. The geophysical measurements include an aeromagnetic survey and thorium (eTh), potassium (K) and uranium (eU) isotope measurements. The results of gamma spectrometer measurements make a distinction between laterite reservoirs. The application of the magnetic and isotope methods allowed the determination of the distribution and development of the laterite crust, as well as the determination of hydrothermal alterations affecting the laterites, which is very useful for mining exploration and exploitation. Such alterations indicate the presence of silicates, which have negative effects on the metallurgic process. It is known that laterite crust has a high content of eU and eTh. From the content of the isotope abundance (eU and eTh) it was possible to infer that Moa laterites were formed before the Mayari Region. From the measurements it was also possible to infer the origin, thickness and age of the lateritic crust.doi: https://doi.org/10.22201/igeof.00167169p.2008.47.2.71  

773.1.#.t: Geofísica Internacional; Vol. 47 Núm. 2: Abril 1, 2008; 99-113

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: 99-113

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

doi: https://doi.org/10.22201/igeof.00167169p.2008.47.2.71

handle: 2dfd52b8fff5d0a3

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

856.#.0.q: application/pdf

file_creation_date: 2008-04-01 16:09:09.0

file_modification_date: 2022-05-27 18:50:21.0

file_creator: Batista J.A.

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245.1.0.b: Geological interpretation of eastern Cuba laterites from an airborne magnetic and radioactive isotope survey

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license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es

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Artículo

Geological interpretation of eastern Cuba laterites from an airborne magnetic and radioactive isotope survey

Batista, J. A.; Blanco, J.; Pérez-flores, M. A.

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, J. A., et al. (2008). Geological interpretation of eastern Cuba laterites from an airborne magnetic and radioactive isotope survey. Geofísica Internacional; Vol. 47 Núm. 2: Abril 1, 2008; 99-113. Recuperado de https://repositorio.unam.mx/contenidos/4132888

Descripción del recurso

Autor(es)
Batista, J. A.; Blanco, J.; Pérez-flores, M. A.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Geological interpretation of eastern Cuba laterites from an airborne magnetic and radioactive isotope survey
Fecha
2008-04-01
Resumen
In eastern Cuba area several geophysical techniques have been applied to distinguish the main geological characteristics of the laterites which are of economical importance for the extraction of iron, nickel and chrome. The geophysical measurements include an aeromagnetic survey and thorium (eTh), potassium (K) and uranium (eU) isotope measurements. The results of gamma spectrometer measurements make a distinction between laterite reservoirs. The application of the magnetic and isotope methods allowed the determination of the distribution and development of the laterite crust, as well as the determination of hydrothermal alterations affecting the laterites, which is very useful for mining exploration and exploitation. Such alterations indicate the presence of silicates, which have negative effects on the metallurgic process. It is known that laterite crust has a high content of eU and eTh. From the content of the isotope abundance (eU and eTh) it was possible to infer that Moa laterites were formed before the Mayari Region. From the measurements it was also possible to infer the origin, thickness and age of the lateritic crust.doi: https://doi.org/10.22201/igeof.00167169p.2008.47.2.71  
Tema
Cortezas lateríticas; exploración de torio y uranio; Cuba; Lateritic crust; thorium and uranium exploration; coherency
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces