Published

2023-11-10

Genesis and Evolution of Pegmatites in Eastern Colombia: Insights from Mineral Chemistry

Génesis y evolución de pegmatitas en el oriente colombiano mediante química mineral

DOI:

https://doi.org/10.15446/esrj.v27n3.102843

Keywords:

Pegmatite, magmatic fractionation, strategic minerals, mineral chemistry (en)
Pegmatita, fraccionamiento magmático, minerales estratégicos, química mineral (es)

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Authors

  • Estefany Andrea Mora-Galindo Universidad Nacional de Colombia
  • Juan Carlos Molano Mendoza Universidad Nacional de Colombia
  • Milton Julián Morales Peña Universidad Nacional de Colombia

 

Pegmatites and granitic intrusives from eastern Colombia, belonging to the Guainía department, were studied to determine the generating magma type, as well as to assess the degree of magmatic fractionation and its relationship with the presence of Nb-Ta-bearing minerals (strategic minerals). To that end, 31 rock samples were studied; EPMA electronic microprobe analyses were conducted on apatite, biotite, garnet, microcline, muscovite, and tourmaline. The results from biotite, garnet, and tourmaline suggest that these rocks originated from a Fe-rich peraluminous melt. 

Moreover, content variation of Ba in microcline, Na in muscovite, Fe-Mg in biotite, and Mn-Sr in apatite, allowed the proposal of a magmatic evolutionary line for these rocks. Nb-Ta-bearing samples were present in the most fractionated rocks where tourmaline and garnet occurred, and thus, were proposed as possible indicators of strategic minerals.

Se estudiaron pegmatitas e intrusivos graníticos del este de Colombia pertenecientes al departamento del Guainía para determinar el tipo de magma generador, su grado de fraccionamiento magmático y su relación con la presencia de minerales portadores de Nb-Ta (minerales estratégicos). Con este propósito, se estudiaron 31 muestras de rocas y se realizaron análisis con microsonda electrónica EPMA en apatito, biotita, granate, microclina, muscovita y turmalina. Los resultados obtenidos a partir de biotita, granate y turmalina sugieren que dichas rocas se generaron a partir de un magma peraluminoso rico en Fe.

Además, la variación del contenido de Ba en la microclina, Na en la muscovita, Fe-Mg en la biotita, y Mn-Sr en el apatito permitió proponer una línea evolutiva magmática para estas rocas. Las muestras portadoras de Nb-Ta estaban presentes en las rocas más fraccionadas, donde se encontraron turmalina y granate, por lo que se propusieron como posibles indicadores de minerales estratégicos.

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Mora-Galindo, E. A., Molano Mendoza, J. C. and Morales Peña, M. J. (2023). Genesis and Evolution of Pegmatites in Eastern Colombia: Insights from Mineral Chemistry. Earth Sciences Research Journal, 27(3), 259–271. https://doi.org/10.15446/esrj.v27n3.102843

ACM

[1]
Mora-Galindo, E.A., Molano Mendoza, J.C. and Morales Peña, M.J. 2023. Genesis and Evolution of Pegmatites in Eastern Colombia: Insights from Mineral Chemistry. Earth Sciences Research Journal. 27, 3 (Nov. 2023), 259–271. DOI:https://doi.org/10.15446/esrj.v27n3.102843.

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(1)
Mora-Galindo, E. A.; Molano Mendoza, J. C.; Morales Peña, M. J. Genesis and Evolution of Pegmatites in Eastern Colombia: Insights from Mineral Chemistry. Earth sci. res. j. 2023, 27, 259-271.

ABNT

MORA-GALINDO, E. A.; MOLANO MENDOZA, J. C.; MORALES PEÑA, M. J. Genesis and Evolution of Pegmatites in Eastern Colombia: Insights from Mineral Chemistry. Earth Sciences Research Journal, [S. l.], v. 27, n. 3, p. 259–271, 2023. DOI: 10.15446/esrj.v27n3.102843. Disponível em: https://revistas.unal.edu.co/index.php/esrj/article/view/102843. Acesso em: 9 aug. 2024.

Chicago

Mora-Galindo, Estefany Andrea, Juan Carlos Molano Mendoza, and Milton Julián Morales Peña. 2023. “Genesis and Evolution of Pegmatites in Eastern Colombia: Insights from Mineral Chemistry”. Earth Sciences Research Journal 27 (3):259-71. https://doi.org/10.15446/esrj.v27n3.102843.

Harvard

Mora-Galindo, E. A., Molano Mendoza, J. C. and Morales Peña, M. J. (2023) “Genesis and Evolution of Pegmatites in Eastern Colombia: Insights from Mineral Chemistry”, Earth Sciences Research Journal, 27(3), pp. 259–271. doi: 10.15446/esrj.v27n3.102843.

IEEE

[1]
E. A. Mora-Galindo, J. C. Molano Mendoza, and M. J. Morales Peña, “Genesis and Evolution of Pegmatites in Eastern Colombia: Insights from Mineral Chemistry”, Earth sci. res. j., vol. 27, no. 3, pp. 259–271, Nov. 2023.

MLA

Mora-Galindo, E. A., J. C. Molano Mendoza, and M. J. Morales Peña. “Genesis and Evolution of Pegmatites in Eastern Colombia: Insights from Mineral Chemistry”. Earth Sciences Research Journal, vol. 27, no. 3, Nov. 2023, pp. 259-71, doi:10.15446/esrj.v27n3.102843.

Turabian

Mora-Galindo, Estefany Andrea, Juan Carlos Molano Mendoza, and Milton Julián Morales Peña. “Genesis and Evolution of Pegmatites in Eastern Colombia: Insights from Mineral Chemistry”. Earth Sciences Research Journal 27, no. 3 (November 10, 2023): 259–271. Accessed August 9, 2024. https://revistas.unal.edu.co/index.php/esrj/article/view/102843.

Vancouver

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Mora-Galindo EA, Molano Mendoza JC, Morales Peña MJ. Genesis and Evolution of Pegmatites in Eastern Colombia: Insights from Mineral Chemistry. Earth sci. res. j. [Internet]. 2023 Nov. 10 [cited 2024 Aug. 9];27(3):259-71. Available from: https://revistas.unal.edu.co/index.php/esrj/article/view/102843

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1. Harold Buitrago, Florian Neumann, Juan Contreras, Carlos A. Vargas. (2024). The thermal structure of the Colombian lithosphere: A regional and basin-scale analysis. Tectonophysics, 885, p.230413. https://doi.org/10.1016/j.tecto.2024.230413.

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