I noted that Acfer 182 (and pairings) are listed as CH2 in Grady's "Catalogue of Meteorites", while it is commonly referred as CH3. Is there any sign of aqueous alteration?
Furthermore, Mount Egerton is listed as anomalous Mesosiderite by Grady, while in many other sources, it is listed as (anomalous, metal rich) Aubrite. Is there some evidence (e.g., O-Isotopes) that Mount Egerton comes from the Aubrite parent body? Thanks for any information, and best greetings, Herbert ______________________________________________ Meteorite-list mailing list [EMAIL PROTECTED] http://www.pairlist.net/mailman/listinfo/meteorite-list
