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Redox systematics of martian magmas with implications for magnetite stability
| Content Provider | NASA Technical Reports Server (NTRS) |
|---|---|
| Author | Danielson, L. Agresti, D. G. Newville, M. Martin, A. M. Morris, R. V. Pando, K. Righter, K. Graff, T. G. Sutton, S. Lanzirotti, A. |
| Copyright Year | 2012 |
| Description | Iron redox systematics of the high FeO shergottitic liquids are poorly known, yet have a fundamental control on stability of phases such as magnetite, ilmenite, and pyroxenes. |
| File Size | 177528 |
| Page Count | 1 |
| File Format | |
| Alternate Webpage(s) | http://archive.org/details/NASA_NTRS_Archive_20120013829 |
| Archival Resource Key | ark:/13960/t91889548 |
| Language | English |
| Publisher Date | 2012-01-01 |
| Access Restriction | Open |
| Subject Keyword | Lunar And Planetary Science And Exploration Stability Shergottites Mars Planet Experimentation Oxidation-reduction Reactions Iron Oxides Magma Mars Volcanoes Ntrs Nasa Technical Reports ServerĀ (ntrs) Nasa Technical Reports Server Aerodynamics Aircraft Aerospace Engineering Aerospace Aeronautic Space Science |
| Content Type | Text |
| Resource Type | Article |