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Updated: Jul 12, 2026

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Combining Solid-state and Solution-based Techniques: Synthesis and Reactivity of Chalcogenidoplumbates(II or IV)
Published on: December 29, 2016
Origen del plomo en las lavas calc-alcalinas andinas, sur del Perú
Resumen
Análisis de isótopos de plomo del sur del Perú.
Área de la Ciencia:
- La geoquímica es la geoquímica.
- Geología de Isótopos Geología de Isótopos.
- Volcanología Volcanología.
Sus antecedentes:
- Las lavas andesíticas en el sur del Perú proporcionan información sobre las interacciones entre la corteza y el manto.
- Comprender el origen de los magmas es crucial para descifrar los procesos tectónicos.
Objetivo del estudio:
- Para investigar la composición isotópica del plomo de lavas andesíticas cuaternarias y gneises precámbricos en el sur del Perú.
- Determinar las fuentes de plomo en la lava andesítica y el papel de los componentes de la corteza.
Principales métodos:
- Análisis de isótopos de plomo de rocas volcánicas (lavas andesíticas) y rocas de la corteza terrestre (gneises granulíticos).
- Aplicación de modelos de mezcla de múltiples componentes para interpretar los datos de isótopos.
Principales resultados:
- Los datos de isótopos de plomo indican una contribución significativa de gneises granulíticos del Precámbrico a las lavas andésticas del Cuaternario.
- El plomo en las lavas puede explicarse por la mezcla entre fuentes derivadas del manto y fuentes de la corteza inferior.
Conclusiones:
- La corteza inferior del Precámbrico es una fuente clave de plomo en los magmas andesíticos del sur del Perú.
- La génesis de magma en esta región implica complejos procesos de mezcla entre el manto y las reservas de la corteza.
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