Origin of EL3 chondrites: Evidence for variable C/O ratios during their course of formation—A state of the art scrutiny
Mineral inventories of enstatite chondrites; (EH and EL) are strictly dictated by combined parameters mainly very low dual oxygen (fO2) and sulfur (fS2) fugacities. They are best preserved in the Almahata Sitta MS‐17, MS‐177 fragments, and the ALHA 77295 and MAC 88136 Antarctic meteorites. These con...
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Veröffentlicht in: | Meteoritics & planetary science 2017-05, Vol.52 (5), p.781-806 |
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