ESTUDIO DE MATERIA ORGÁNICA INSOLUBLE EN METEORITO CARBONÁCEO AGUAS ZARCAS
DOI:
https://doi.org/10.47820/recima21.v4i2.2695Palabras clave:
condritas carbonáceas CM2; geoquímica orgánica; meteoritos; partículas orgánicas; kerógeno.Resumen
A través de la correlación de datos analíticos, el estudio geoquímico y la microscopía óptica orgánica permiten indicar las condiciones y el estado de conservación de los insumos orgánicos dispersos en las rocas sedimentarias, señalando el ambiente y los procesos geotérmicos y físicos que los afectaron durante las distintas etapas evolutivas post-entierro. . Análogamente, en la materia orgánica contenida en la matriz de meteoritos carbonosos se aplicó la misma metodología convencional. Con base en estos supuestos, observamos que el aislado orgánico insoluble del meteorito carbonáceo Aguas Zarcas exhibe una morfografía similar a los productos secundarios resultantes de procesos intermedios de maduración térmica sedimentaria. A partir de la caracterización del perfil orgánico, nuestro artículo sugiere una correspondencia sobre las posibles condiciones deposicionales, térmicas y de conservación de las partículas orgánicas en el cuerpo parental de origen de los fragmentos cósmicos.
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