EARLY CRUSTAL EVOLUTION OF MARS 1
By F. Nimmo. 2005
244 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science
View Paper: https://www.semanticscholar.org/paper/b213a6234bb52448addb3f155b8663c1e63924a4
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In Astronomy and Astrophysics
- L. Elkins‐Tanton
- Stuart J. Robbins
- Bethany L. Ehlmann
- E. Parmentier
- J. Bibring
- William Bottke
- Yves Langevin
- J. Roberts
In Atmospheric Science
- L. Elkins‐Tanton
- Stuart J. Robbins
- William Bottke
- R. Lillis
- E. Parmentier
- P. C. Hess
- B. Hynek
- M. Hoke
Citations in the corpus
- Possible formation of ancient crust on Mars through magma ocean processes (2005, methodology): “MER data compiled by Nimmo and Tanaka [2005]).”
- Updated global map of Martian valley networks and implications for climate and hydrologic processes (2010, background): “Lower solar luminosity with a high EUV flux, Mars’s distance from the sun, and a dynamo that shut off before 4.0 Ga [ Nimmo and Tanaka, 2005 ] conflict with a warm and wet early Mars [e.g., Kasting 1991; Segura et al., 2008; Tian et al., 2009].”
- Degree-1 convection in the Martian mantle and the origin of the hemispheric dichotomy (2006, background): “[53] How rapidly a degree-1 structure can form is important for understanding the crustal dichotomy, given that the dichotomy may have formed in the early Noachian or earlier [Frey et al., 2002; Nimmo and Tanaka, 2005; Solomon et al., 2005].”
- Large impact crater histories of Mars: The effect of different model crater age techniques (2013, methodology): “The main literature comparis ons quote ages to the 1 or 10 Myr level (Nimmo and Tanaka, 2005; Werner, 2008; Fassett and Head, 2011 ); specific ages in this paper are given to the 10 Myr level while combined results are given to the 100 Myr level – however, it is recognized that the inherent…”
- The Sedimentary Rock Record of Mars: Distribution, Origins, and Global Stratigraphy (2012, unknown): “…apply: a relative sequence of superimposed and cross-cutting rocks (terrains with distinct properties) is established (Scott and Tanaka 1986, Greeley and Guest 1987, Nimmo and Tanaka 2005), and this record is then calibrated in ‘‘absolute’’ time using crater counting (Hartmann and Neukum 2001).”
- Constraints on the depths and temperatures of basaltic magma generation on Earth and other terrestrial planets using new thermobarometers for mafic magmas (2009, background): “(Chen and Wasserburg, 1986; Borg et al.,1997; Blichert-Toft et al.,1999; Bouvier et al., 2005; Nimmo and Tanaka, 2005 )).”