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Updated: Sep 10, 2025

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La fuente y el conductor térmico del volcanismo lunar joven (<3,0 Ga)

Chengyuan Wang1, Yuqi Qian2,3, Jintuan Wang1

  • 1State Key Laboratory of Deep Earth Processes and Resources, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China.

Science advances
|August 22, 2025
PubMed
Resumen

El volcanismo lunar joven, particularmente después del período Imbriano, se explica por la capa subterránea magmática. Este proceso, que involucra a la capa de acumulado con ilmenita (IBC), impulsó el magmatismo lunar prolongado y explica las diferencias de composición en los basaltos en la Luna.

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