登陆火星，我们会看到什么？
The following article is from 星球研究所 Author 星球研究所
火星已经几乎死去
[1] Moser, D.E., Arcuri, G.A., Reinhard, D.A. et al. Decline of giant impacts on Mars by 4.48 billion years ago and an early opportunity for habitability. Nat. Geosci. 12, 522–527 (2019).
[2] Citron R I, Manga M, Tan E. A hybrid origin of the Martian crustal dichotomy: degree-1 convection antipodal to a giant impact[J]. Earth and Planetary Science Letters, 2018, 491: 58-66.
[3] Nimmo F, Hart S D, Korycansky D G, et al. Implications of an impact origin for the martian hemispheric dichotomy[J]. Nature, 2008, 453(7199): 1220-1223.
[4] Irwin III R P, Watters T R. Geology of the Martian crustal dichotomy boundary: Age, modifications, and implications for modeling efforts[J]. Journal of Geophysical Research: Planets, 2010, 115(E11).
[5] Leone G, Tackley P J, Gerya T V, et al. Three‐dimensional simulations of the southern polar giant impact hypothesis for the origin of the Martian dichotomy[J]. Geophysical research letters, 2014, 41(24): 8736-8743.
[6] Marinova M M, Aharonson O, Asphaug E. Mega-impact formation of the Mars hemispheric dichotomy[J]. Nature, 2008, 453(7199): 1216-1219.
[7] Bouvier L C, Costa M M, Connelly J N, et al. Evidence for extremely rapid magma ocean crystallization and crust formation on Mars[J]. Nature, 2018, 558(7711): 586-589.
[8] Frey H V. Impact constraints on, and a chronology for, major events in early Mars history[J]. Journal of Geophysical Research: Planets, 2006, 111(E8).
[9] The Planetary and Space Science Centre, EARTH IMPACT DATABASE
[10] Frey H V. Impact constraints on, and a chronology for, major events in early Mars history[J]. Journal of Geophysical Research: Planets, 2006, 111(E8).
[11] Robbins S J , Hynek B M . A new global database of Mars impact craters ≥1 km: 1. Database creation, properties, and parameters[J]. Journal of Geophysical Research Planets, 2012, 117(E5).
[12] Therriault A M, Grieve R A F, Reimold W U. Original size of the Vredefort Structure: Implications for the geological evolution of the Witwatersrand Basin[J]. Meteoritics & Planetary Science, 1997, 32(1): 71-77.
[13] Zimbelman J R, Garry W B, Bleacher J E, et al. Volcanism on Mars[M]//The Encyclopedia of Volcanoes. Academic Press, 2015: 717-728.
[14] Xiao L, Huang J, Christensen P R, et al. Ancient volcanism and its implication for thermal evolution of Mars[J]. Earth and Planetary Science Letters, 2012, 323: 9-18.
[15] Grott M, Baratoux D, Hauber E, et al. Long-term evolution of the Martian crust-mantle system[J]. Space Science Reviews, 2013, 174(1): 49-111.
[16] Orr T R, Bleacher J E, Patrick M R, et al. A sinuous tumulus over an active lava tube at Kīlauea Volcano: Evolution, analogs, and hazard forecasts[J]. Journal of Volcanology and Geothermal Research, 2015, 291: 35-48.
[17] Horvath D G, Moitra P, Hamilton C W, et al. Evidence for geologically recent explosive volcanism in Elysium Planitia, Mars[J]. arXiv preprint arXiv:2011.05956, 2020.
[18] Yoshida H, Hasegawa H, Katsuta N, et al. Fe-oxide concretions formed by interacting carbonate and acidic waters on Earth and Mars[J]. Science advances, 2018, 4(12): eaau0872.
[19] Matsubara Y, Howard A D, Burr D M, et al. River meandering on Earth and Mars: A comparative study of Aeolis Dorsa meanders, Mars and possible terrestrial analogs of the Usuktuk River, AK, and the Quinn River, NV[J]. Geomorphology, 2015, 240: 102-120.
[20] Di Achille G, Hynek B M. Ancient ocean on Mars supported by global distribution of deltas and valleys[J]. Nature Geoscience, 2010, 3(7): 459-463.
[21] Citron R I, Manga M, Hemingway D J. Timing of oceans on Mars from shoreline deformation[J]. Nature, 2018, 555(7698): 643-646.
[22] Duran S, Coulthard T J. The Kasei Valles, Mars: a unified record of episodic channel flows and ancient ocean levels[J]. Scientific reports, 2020, 10(1): 1-7.
[23] Nahm A L, Schultz R A. Evaluation of the orogenic belt hypothesis for the formation of the Thaumasia Highlands, Mars[J]. Journal of Geophysical Research: Planets, 2010, 115(E4).
[24] Stern R J, Gerya T, Tackley P J. Stagnant lid tectonics: Perspectives from silicate planets, dwarf planets, large moons, and large asteroids[J]. Geoscience Frontiers, 2018, 9(1): 103-119.
[25] Palin R M, Santosh M, Cao W, et al. Secular metamorphic change and the onset of plate tectonics[J]. Earth-Science Reviews, 2020: 103172.
[26] Mittelholz A, Johnson C L, Feinberg J M, et al. Timing of the martian dynamo: New constraints for a core field 4.5 and 3.7 Ga ago[J]. Science Advances, 2020, 6(18): eaba0513.
[27] Day M, Kocurek G. Observations of an aeolian landscape: From surface to orbit in Gale Crater[J]. Icarus, 2016, 280: 37-71.
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