Oxygen fugacity of martian basalts from electron microprobe oxygen and TEM-EELS analyses of Fe-Ti oxides
By C. Herd, J. Papike, A. Brearley. 2001
144 citations recorded by the source corpus.
Subfields: Geophysics, Molecular Biology
View Paper: https://www.semanticscholar.org/paper/b8db4201d55cec53fdd6eff32a72c8fe9e5b2760
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In Geophysics
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Citations in the corpus
- Experimental petrology of the basaltic shergottite Yamato‐980459: Implications for the thermal structure of the Martian mantle (2006, background): “The other depleted shergottites include Queen Alexandra Range 94201, DaG 476, and SaU 005 (e.g., Borg et al. 1997, 2003; Herd et al. 2001; Herd 2003).”
- The oxygen fugacity of olivine‐phyric martian basalts and the components within the mantle and crust of Mars (2003, methodology): “For this reason, others have questioned whether the fO2 estimates of Herd et al. (2001) reflect the conditions under which the magma began to crystallize (Wadhwa 2001), although Herd et al. (2001) present arguments to the contrary.”