Photochemical Escape of Oxygen from Early Mars
Jinjin Zhao, Feng Tian Icarus doi:10.1016/j.icarus.2014.12.032 available online 6 January 2015 LINK
Highly siderophile element (HSE) abundances in the mantle of Mars are due to core formation at high pressure and temperature
K. Righter, L. R. Danielson, K. M. Pando, J. Williams, M. Humayun, R. L. Hervig and T. G. Sharp Meteoritics & Planetary Science. doi: 10.1111/maps.12393 LINK
Siderophile and chalcophile element abundances in shergottites: Implications for Martian core formation
Shuying Yang, Munir Humayun, Kevin Righter, Gwendolyn Jefferson, Dana Fields and Anthony J. Irving Meteoritics & Planetary Science. doi: 10.1111/maps.12384 LINK
Meteoritical Bulletin updates
- 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)
- Caleta el Cobre 081 (L3)
- Calate 064 (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)
