What is controlling the reflectance spectra (0.35- 150 µm) of hydrated (and dehydrated) carbonaceous chondrites?
· by karmaka · in carbonaceous chondrite, CM, CR, thermal metamorphism
Pierre Beck, A. Maturilli, A. Garenne, P. Vernazza, J. Helbert, E. Quirico, B. Schmitt Icarus In Press, Accepted Manuscript, Available online 17 May 2018 LINK “Highligths • The 0.7 µm feature in hydrated carbonaceous chondrites…
| M | T | W | T | F | S | S |
|---|---|---|---|---|---|---|
| 1 | 2 | 3 | 4 | |||
| 5 | 6 | 7 | 8 | 9 | 10 | 11 |
| 12 | 13 | 14 | 15 | 16 | 17 | 18 |
| 19 | 20 | 21 | 22 | 23 | 24 | 25 |
| 26 | 27 | 28 | 29 | 30 | ||
Archives
METEORITICAL BULLETIN UPDATE
-
Northwest Africa 15923 (Eucrite-melt breccia)
-
Northwest Africa 15920 (LL3)
-
Northwest Africa 15917 (Martian (shergottite))
-
Calama 391 (H3)
-
Calama 389 (H3)
-
Calama 374 (H3)
-
Limón Verde 024 (H3)
-
Calama 370 (H3)
-
Northwest Africa 15910 (Martian (shergottite))
-
Northwest Africa 15909 (Ureilite)
-
Northwest Africa 15886 (Eucrite)
-
Reggane 005 (CK5)
-
Plateau du Tademait 011 (Eucrite-pmict)
-
Northwest Africa 15849 (Eucrite-br)
-
Northwest Africa 15850 (Eucrite)
