The oxygen fugacity of olivine‐phyric martian basalts and the components within the mantle and crust of Mars
By C. Herd. 2003
161 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science, Geophysics
View Paper: https://www.semanticscholar.org/paper/a634e153bea6bd5ac4620da39fdc4d85b8c5f644
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Citations in the corpus
- Bulk composition and early differentiation of Mars (2007, unknown): “al., 1997, 2003; Herd et al., 2002; Herd, 2003; Goodrich et al., 2003; Borg and Draper, 2003; McLennan, 2003].”
- A hydrogen-based oxidation mechanism relevant to planetary formation (2013, unknown): “5 (Herd, 2003; Herd et al., 2002; McCubbin et al., 2013; Shearer et al., 2013; Wadhwa, 2001).”
- The sulfur content of volcanic gases on Mars (2009, background): “If such magmas, whose redox condition and H2O content are within the range expected for Mars basalts ([Herd et al., 2002], [Herd, 2003], [Righter et al., 2007] and [Wadhwa, 2001]), constituted the dominant part of the Tharsis province, then we do not expect any exceptionally high sulfur delivery…”
- 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).”