The most primitive CM chondrites, Asuka 12085, 12169, and 12236, of subtypes 3.0–2.8: Their characteristic features and classification
· by karmaka · in aqueous alteration, carbonaceous chondrite, CM, OSIRIS-REx / 101955 Bennu, thermal metamorphism
M. Kimura, N. Imae, M. Komatsu, J. A. Barrat, R.C.Greenwood, A.Yamaguchi, T.Noguchi Polar Science In Press, Journal Pre-proof. Available online 13 August 2020, 100565 LINK “CM chondrites (CMs) are the most abundant group of carbonaceous…
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- Northwest Africa 18584 (Eucrite)
- Northwest Africa 18582 (Eucrite-br)
- Northwest Africa 18578 (L3)
- Northwest Africa 18581 (Eucrite)
- Northwest Africa 18576 (LL3-4)
- Northwest Africa 18520 (CVox3)
- Los Vientos 600 (Ureilite-an)
- Northeast Africa 124 (Ureilite)
- Northwest Africa 18439 (Lunar)
- Northwest Africa 18256 (L3)
- Northwest Africa 18231 (Martian (shergottite))
- Northwest Africa 18560 (LL3)
- Calate 064 (L3)
- Caleta el Cobre 081 (L3)
- Catalina 1052 (L3)
- Denader 004 (CB)
- Fengning (Iron, IIIAB)
- Mdeïné 003 (Iron, ungrouped)
- Northwest Africa 16442 (L3-5-melt breccia)
- Gyarub Zangbo (b) (Iron, IAB-sHH)


































