The Akkaya-Feke (Adana-Turkey) Assessment Of The Relationship Between Fluorite And Rare Earth Elements (REE) IDW And Satellite-Based Tectonic Lineaments

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Sinan Altuncua
Ramazan Demircioğlu

Resumen

El área de estudio se encuentra en la sección central de Tauride, una unidad tectónica de Turquía. Esta región abarca el pueblo de Akkaya (Feke-Adana) junto con las zonas circundantes de la provincia de Adana. La región ha experimentado una deformación polifásica, lo que ha dado lugar a fallas y fracturas que proporcionan los lugares adecuados para la mineralización. Además, el magmatismo ha contribuido a la formación de diversos yacimientos minerales. Entre estos minerales se encuentra la fluorita, que se utiliza ampliamente en las industrias metalúrgica, química y del vidrio. El objetivo de este estudio es investigar la mineralización de fluorita y la distribución de elementos de tierras raras (REE) utilizando el método de ponderación inversa de la distancia (IDW), así como evaluar la relación entre las líneas tectónicas basadas en satélites y la mineralización. Los resultados sugieren que la mineralización de fluorita de tipo veta y la distribución de los elementos de tierras raras están generalmente alineados con los lineamientos tectónicos identificados.

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Cómo citar
Altuncua, S., & Demircioğlu, R. (2026). The Akkaya-Feke (Adana-Turkey) Assessment Of The Relationship Between Fluorite And Rare Earth Elements (REE) IDW And Satellite-Based Tectonic Lineaments. Geofísica Internacional, 65(2), 2147–2160. https://doi.org/10.22201/igeof.2954436xe.2026.65.2.1946
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