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Petrogenesis of magmatic dropstones in the Bushveld Complex: Implications for magma chamber growth and evolution
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DOI:10.1016/j.lithos.2026.108691.png)
Abstract
En 中文
• Magmatic dropstones identified in the Bushveld Complex. • Blocks are fragments of roof-grown melanoritic rocks. • Fine grains formed by thermal recrystallization during replenishment. • Dropstones impacted a coherent cumulate floor.
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