^Cordell, B. 1984. A Preliminary Assessment of Martian Natural Resource Potential. The Case For Mars II.
^Clark, B. 1984. Chemistry of the Martian Surface: Resources for the Manned Exploration of Mars, in The Case For Mars. P. Boston, ed. American Astronautical Society. Univelt Inc. San Diego, CA
^West, M., J. Clarke. 2010. Potential martian mineral resources: Mechanisms and terrestrial analogs. Planetary and Space Science 58, 574–582.ResearchGate (页面存档备份,存于互联网档案馆)
^Laimin, Zhu. A study on the relations between Ultrabasic Dikes and fine disseminated gold deposits in southwestern Guizhou Province as exemplified by Zimudang large-sized gold deposit. Chinese Journal of Geochemistry. 1998, 17 (4): 362–371. S2CID 130661251. doi:10.1007/bf02837988.
^Pirajno, F. 2004. Metallogeny in the Capricorn Orogen, Western Australia, the result of multiple ore-forming processes. Precambrian Research: 128. 411-439
^David Susko, Suniti Karunatillake, Gayantha Kodikara, J. R. Skok, James Wray, Jennifer Heldmann, Agnes Cousin, Taylor Judice. "A record of igneous evolution in Elysium, a major martian volcanic province. Scientific Reports, 2017; 7: 43177 doi:10.1038/srep43177
^Head, J. et al. 2006. The Huygens-Hellas giant dike system on Mars: Implications for Late Noachian-Early Hesperian volcanic resurfacing and climate evolution. Geology: 34. 285-288.
^Goudy, C. and R. Schultz. 2005. Dike intrusions beneath grabens south of Arsia Mons, Mars. Geophysical Research Letters: 32. L05201
^Mege, D. et al. 2003. Volcanic rifting at Martian grabens. Journal of Geophysical Research: 108.
^Wilson, L. and J. Head. 2002. Tharsis-radial graben systems as the surface manifestation of plume-related dike intrusion complexes: Models and implications. Journal of Geophysical Research: 107.
^Crisp, J. 1984. Rates of magma emplacement and volcanic output. J. Volcano. Geotherm. Res: 20. 177-211.
^Ernst, R. 2007. large Igneous Provinces in Canada Through Time and Their Metallogenic Potential. Mineral Deposits of Canada: A Synthesis of Major Deposit-Types, District Metallogeny, the Evolution of Geological Provinces, and Exploration Methods: Geological Association of Canada, Mineral Division, Special Publication No. 5. 929-937.
^ 25.025.125.2Grieve, R., V. Masaitis. 1994. The Economic Potential of Terrestrial Impact Craters. International Geology Review: 36, 105-151.
^Osinski, G, J. Spray, and P. Lee. 2001. Impact-induced hydrothermal activity within the Haughton impact structure, Arctic Canada: Generation of a transient, warm, wet oasis. Meteoritics & Planetary Science: 36. 731-745
^Pirajno, F. 2000. Ore Deposits and Mantle Plumes. Kluwer Academic Publishers. Dordrecht, The Netherlands
^Head, J. and J. Mustard. 2006. Breccia Dikes and Crater-Related Faults in Impact Craters on Mars: Erosion and Exposure on the Floor of a 75-km Diameter Crater at the Dichotomy Boundary. Special Issue on Role of Volatiles and Atmospheres on Martian Impact Craters Meteoritics & Planetary Science
^Arvidson, R., et al. 2015. Recent Results from the Opportunity Rover's Exploration of Endeavour Crater, Mars. 46th Lunar and Planetary Science Conference. 1118.pdf
^Crumpler, L., R. Arvidson, W. Farrand, M. Golombek, J. Grant, D. Ming, D. Mittlefehldt, T. Parker. 2015. Opportunity In Situ Geologic Context of Aqueous Alteration Along Offsets in the Rim of Endeavour Crater. 46th Lunar and Planetary Science Conference. 2209.pdf
^Grieve R., A. Therriault. 2000 Vredefort, Sudbury, Chicxulub: Three of a kind? Annual Review of Earth and Planetary Sciences 28: 305-338 Grieve
^Carrozzo, F. et al. 2017. Geology and mineralogy of the Auki Crater, Tyrrhena Terra, Mars: A possible post-impact-induced hydrothermal system. 281: 228-239
^Loizeau, D. et al. 2012. Characterization of hydrated silicate-bearing outcrops in Tyrrhena Terra, Mars: implications to the alteration history of Mars. Icarus: 219, 476-497.
^Naumov, M. 2005. Principal features of impact-generated hydrothermal circulation systems: mineralogical and geochemical evidence. Geofluids: 5, 165-184.
^Ehlmann, B., et al. 2011. Evidence for low-grade metamorphism, hydrothermal alteration, and diagenesis on Mars from phyllosilicate mineral assemblages. Clays Clay Miner: 59, 359-377.
^Osinski, G. et al. 2013. Impact-generated hydrothermal systems on Earth and Mars. Icarus: 224, 347-363.
^Schwenzer, S., D. Kring. 2013. Alteration minerals in impact-generated hydrothermal systems – Exploring host rock variability. Icarus: 226, 487-496.
^Marzo, G., et al. 2010. Evidence for Hesperian impact-induced hydrothermalism on Mars. Icarus: 667-683.
^Mangold, N., et al. 2012. Hydrothermal alteration in a late Hesperian impact crater on Mars. 43rd Lunar and Planetary Science. #1209.
^Tornabene, L., et al. 2009. Parautochthonous megabreccias and possible evidence of impact-induced hydrothermal alteration in Holden crater, Mars. 40th LPSC. #1766.
^H. G. Changela and J. C. Bridges. Alteration assemblages in the nakhlites: Variation with depth on Mars. Meteoritics & Planetary Science, 2011 45(12):1847-1867 doi:10.1111/j.1945-5100.2010.01123.x
^Squyres, et al. 2004. The Opportunity Rover's Athena science investigation at Meridiani Planum. Science: 306. 1598-1703.
^Rodionov, D. et al. 2005. An iron-nickel meteorite on Meridiani Planum: observations by MER Opportunity's Mossbauer Spectrometer, European Geosciences Union in Geophysical Research Abstracts: 7. 10242
^Yen, A., et al. Nickel on Mars: constraints on meteoritic material at the surface. Journal of Geophysical Research-Planets: 111. E12S11
^Landis, G. 2009. Meteoritic steel as a construction resource on Mars. Acta Astronautica: 64. 183-187.
^Ruzicka, G. et al. 2001. Comparative geochemistry of basalts from the Moon, Earth, HED asteroid, and Mars: implications for the origin of the Moon. Geochimica et Cosmochimica ACTA: 65. 979-997.
^ 55.055.1West, M. and J. Clarke. 2010. Potential martian mineral resources: Mechanisms and terrestrial analogs. Planetary and Space Science: 58. 574-582. ResearchGate (页面存档备份,存于互联网档案馆)