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January 1, 2025Петрология / Petrology

Origin of the Earth’s first felsic material: a hydrogen perspective?

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Authors

LAL. Ya. Aranovich

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Implication

Analysis reveals fractional crystallization effects on felsic material in basalt and enstatite chondrite, suggesting zircon formation processes.

Key Points

  • Felsic material formed from interactions of magma with a hydrogen atmosphere.
  • Zircon crystallizes between 730 and 750°C during the differentiation of enstatite chondrite.
  • Fractional crystallization processes were assessed through experimental melting models of basalt komatiite and enstatite chondrite.
  • Findings highlight complex internal processes impacting early Earth material evolution.

Cite This Study

L. Ya. Aranovich (2025) studied this question.

synapsesocial.com/papers/69255737c0ce034ddc35ad13https://doi.org/10.7868/s3034585525010044
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Also Consider

Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context:

  1. 1The solubility of molecular hydrogen in silicate melts and the origin of hydrogen in the interiors of terrestrial planets2025
  2. 2Melting experiments and the origins of felsic crust on early Earth2026
  3. 3Thermochemical models of early Earth evolution constrained by geochemical data2024
  4. 4Earliest Evolved Rocks: A Solar System Perspective2026
  5. 5The Silicate Bridge: Low-Pressure Percolation, Inherited Redox, and the Onset of the Anoxic Iron-Silicate Ocean2026