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Leone, Giovanni (2016-01-01). "Alignments of volcanic features in the southern hemisphere of Mars produced by migrating mantle plumes". Journal of Volcanology and Geothermal Research. 309: 78–95. Bibcode:2016JVGR..309...78L. doi:10.1016/j.jvolgeores.2015.10.028.
Baker, D.; et al. (2010). "Flow patterns of lobate debris aprons and lineated valley fill north of Ismeniae Fossae, Mars: Evidence for extensive mid-latitude glaciation in the Late Amazonian". Icarus. 207 (1): 186–209. Bibcode:2010Icar..207..186B. doi:10.1016/j.icarus.2009.11.017.
Golabek, Gregor J.; Keller, Tobias; Gerya, Taras V.; Zhu, Guizhi; Tackley, Paul J.; Connolly, James A.D. (September 2011). "Origin of the martian dichotomy and Tharsis from a giant impact causing massive magmatism". Icarus. 215 (1): 346–357. doi:10.1016/j.icarus.2011.06.012.
Frey, H.; Schultz, R.A. (1988). "Large impact basins and the mega-impact origin for the crustal dichotomy of Mars". Geophys. Res. Lett. 15 (3): 229–232. Bibcode:1988GeoRL..15..229F. doi:10.1029/gl015i003p00229.
Frey, H.; Schultz, R.A. (1988). "Large impact basins and the mega-impact origin for the crustal dichotomy of Mars". Geophys. Res. Lett. 15 (3): 229–232. Bibcode:1988GeoRL..15..229F. doi:10.1029/gl015i003p00229.
Clancy, R. T.; Grossman, A. W.; et al. (Jul 1996). "Water Vapor Saturation at Low Altitudes around Mars Aphelion: A Key to Mars Climate?". Icarus. 122 (1): 36–62. Bibcode:1996Icar..122...36C. doi:10.1006/icar.1996.0108.
Leone, Giovanni (2014-05-01). "A network of lava tubes as the origin of Labyrinthus Noctis and Valles Marineris on Mars". Journal of Volcanology and Geothermal Research. 277: 1–8. Bibcode:2014JVGR..277....1L. doi:10.1016/j.jvolgeores.2014.01.011.
Leone, Giovanni (2016-01-01). "Alignments of volcanic features in the southern hemisphere of Mars produced by migrating mantle plumes". Journal of Volcanology and Geothermal Research. 309: 78–95. Bibcode:2016JVGR..309...78L. doi:10.1016/j.jvolgeores.2015.10.028.
Baker, D.; et al. (2010). "Flow patterns of lobate debris aprons and lineated valley fill north of Ismeniae Fossae, Mars: Evidence for extensive mid-latitude glaciation in the Late Amazonian". Icarus. 207 (1): 186–209. Bibcode:2010Icar..207..186B. doi:10.1016/j.icarus.2009.11.017.
Frey, H.; Schultz, R.A. (1988). "Large impact basins and the mega-impact origin for the crustal dichotomy of Mars". Geophys. Res. Lett. 15 (3): 229–232. Bibcode:1988GeoRL..15..229F. doi:10.1029/gl015i003p00229.
Frey, H.; Schultz, R.A. (1988). "Large impact basins and the mega-impact origin for the crustal dichotomy of Mars". Geophys. Res. Lett. 15 (3): 229–232. Bibcode:1988GeoRL..15..229F. doi:10.1029/gl015i003p00229.
Clancy, R. T.; Grossman, A. W.; et al. (Jul 1996). "Water Vapor Saturation at Low Altitudes around Mars Aphelion: A Key to Mars Climate?". Icarus. 122 (1): 36–62. Bibcode:1996Icar..122...36C. doi:10.1006/icar.1996.0108.