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Magmatic Irons.pdf

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Preview of Magmatic Irons
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Summary

Enon and Puente del Zacate are reevaluated as IIIAB silicate-bearing irons, with Enon's oxygen isotope composition matching the IIIAB chromite value, and both occupying the same part of the crystallization trend defined by the IIIAB iron group, suggesting they formed at the same time in the fractional crystallization history of the IIIAB core, with possible origins including metamorphosed chondrites or partial melt residues, but not IAB-like models.

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Enon and Puente del Zacate are reevaluated as IIIAB silicate-bearing irons, with Enon's oxygen isotope composition matching the IIIAB chromite value, and both...

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  • File Format: PDF
  • File Size: 156 KB
  • Pages: 2
  • Language: EN
  • Total Downloads: 153
  • Last Updated: 3 weeks ago

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