Jiddat al Harasis 422: A ureilite with an extremely high degree of shock melting
Version of Record online: 24 JAN 2011
© The Meteoritical Society, 2011
Meteoritics & Planetary Science
Volume 46, Issue 1, pages 134–148, January 2011
How to Cite
JANOTS, E., GNOS, E., HOFMANN, B. A., GREENWOOD, R. C., FRANCHI, I. A. and BISCHOFF, A. (2011), Jiddat al Harasis 422: A ureilite with an extremely high degree of shock melting. Meteoritics & Planetary Science, 46: 134–148. doi: 10.1111/j.1945-5100.2010.01161.x
- Issue online: 11 FEB 2011
- Version of Record online: 24 JAN 2011
- (Received 15 April 2009; revision accepted 17 September 2010)
Table S1. Electron microprobe analyses of the olivine in the matrix.
Table S2. Representative EMP analyses of the olivine in the clast.
Table S3. Electron microprobe analyses of the orthopyroxene in the clast veins.
Table S4. Electron microprobe analyses of the orthopyroxene in the matrix.
Table S5. Electron microprobe analyses of the clinopyroxene in the matrix and the clasts.
Table S6. Electron microprobe analyses of chromite.
Table S7. Scanning electron microscope analyses, using EDS detector, of felsic material and SiO2-rich phase in the matrix.
Figure S1. Plot of δ18O vs Δ17O showing the oxygen isotope composition of the JaH 422 treated matrix sample and dunite clast and untreated matrix in relation to other major achondrite groups.
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