Geochemical characterization of scoriaceous and unmelted micrometeorites from the Sør Rondane Mountains, East Antarctica: Links to chondritic parent bodies and the effects of alteration Vrije Universiteit Brussel
Micrometeorites originate from the interplanetary dust complex and continuously fall to the Earth's surface in large amounts. About 10 to 20% of micrometeorites are not melted upon reaching the Earth's surface, preserving the primary features and characteristics of the parent material. Consequently, unmelted micrometeorites, together with scoriaceous micrometeorites, an intermediate form between cosmic spherules and unmelted micrometeorites, ...