Ventilation of CO2 from a reduced mantle and consequences for the early Martian greenhouse
By M. Hirschmann, A. Withers. 2008
134 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Geophysics, Paleontology
View Paper: https://www.semanticscholar.org/paper/0818ec2a998d205114f4401b5c07536a3eb2cb7d
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The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Astronomy and Astrophysics
- R. Wordsworth
- Francois Forget
- Ehouarn Millour
- J. Leconte
- Jean-Baptiste Madeleine
- H. Lammer
- Matthias Grott
- R. Haberle
In Geophysics
- R. Wordsworth
- H. Lammer
- Matthias Grott
- A. Morschhauser
- Ernst Hauber
- J. Leconte
- L. Elkins‐Tanton
- O. Mousis
In Paleontology
Citations in the corpus
- The sulfur content of volcanic gases on Mars (2009, unknown): “Keywords: Mars; sulfur; basalt; volcanic degassing; redox; mantle; atmosphere”
- Outgassing History and Escape of the Martian Atmosphere and Water Inventory (2015, methodology): “Combining the chemical model for CO2 solubility (Hirschmann and Withers 2008) with parameterized thermal evolution models (Morschhauser et al.”
- 3D modelling of the early Martian Climate under a denser CO2 atmosphere: Temperatures and CO2 ice clouds. (2012, methodology): “In particular, Hirschmann and Withers (2008) calculated that post-4.”
- Magma oceans in the inner solar system (2012, background): “Hirschmann & Withers (2008) extended this work to show that, rather than degassing, a magma ocean in equilibrium with graphite retains significant portions of the planet’s carbon budget in its solidifying interior.”
- A hydrogen-based oxidation mechanism relevant to planetary formation (2013, background): “f (O2) estimates from text and (Herd 2003, 2006; Herd et al., 2002; Herd and Papike, 2000; Hirschmann and Withers, 2008; McCubbin et al., 2009; Righter and Drake, 1996; Righter et al., 2008; Sarbadhikari et al., 2009, 2011; Steele et al., 2012; Wadhwa 2001, 2008).”
- Transient reducing greenhouse warming on early Mars (2016, unknown): “as the sole source of reduced gases, however, is that a mantle reducing enough to outgas sucient H 2 directly would outgas CO 2 less eciently, instead retaining large amounts of carbon in the melt [Hirschmann and Withers, 2008; Wetzel et al., 2013]. A third potential reduced gas source is CH 4 and H”