Andi Koppelt
4/6/2018 12:17:27 PM |
Cool pattern - like ice crystals. |
Bernd Pauli
4/6/2018 11:21:03 AM |
McCOY T.J. (1995) Silicate-bearing IIE irons: Early mixing and differentiation in a core-mantle environment and shock resetting of ages (abs. Meteoritics 30-5, 1995, 542-543): ... The chondritic precursor was probably not identical to H chondrites. |
Bernd Pauli
4/6/2018 11:19:03 AM |
CLARKE R.S. Jr. et al. (1992) Clues to the developmental and disintegration history of the Watson (and probably also the Kodaikanal) IIE iron meteorite parent body (Meteoritics 27-3, 1992, A210):
The Watson iron meteorite contains a large silicate mass of H-group composition, igneous texture, and of IIE oxygen isotopes linking anew the IIEs and the H chondrites. |
Anne Black
4/6/2018 10:02:34 AM |
Thank you Reporter-Paul! |
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