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New Perspectives on Ancient Mars
Open accessAbstract
Mars was most active during its first billion years. The core, mantle, and crust formed within â¼50 million years of solar system formation. A magnetic dynamo in a convecting fluid core magnetized the crust, and the global field shielded a more massive early atmosphere against solar wind stripping. The Tharsis province became a focus for volcanism, deformation, and outgassing of water and carbon dioxide in quantities possibly sufficient to induce episodes of climate warming. Surficial and near-surface water contributed to regionally extensive erosion, sediment transport, and chemical alteration. Deep hydrothermal circulation accelerated crustal cooling, preserved variations in crustal thickness, and modified patterns of crustal magnetization.
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“If plate tectonics ever initiated at all, it ceased rapidly (Connerney et al. 2001; Solomon et al. 2005).”
From The Climate of Early Mars (2016) · cites this paper as Solomon et al. 2005
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Self-citation
Metadata
- Authors
- Solomon, S. C., Aharonson, O., Aurnou, J. M., Banerdt, W. B., Carr, M. H., Dombard, A. J., Frey, H. V., Golombek, M. P., Hauck, S. A., Head, J. W., Jakosky, B. M., Johnson, C. L., McGovern, P. J., Neumann, G. A., Phillips, R. J., Smith, D. E., & Zuber, M. T.
- Affiliations
- California Institute of Technology (US)
- Corresponding author
- Solomon, Sean C.
- ORCID
- Venue
- Science
- Published
- 2005-02-25
- Volume
- 307
- Issue
- 5713
- Pages
- 1214-1220
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2110777688
- Cited by
- 316
- References
- 97
- Citations by year
- 2026: 5 · 2025: 13 · 2024: 8 · 2023: 13 · 2022: 14 · 2021: 10 · 2020: 9 · 2019: 7 · 2018: 13 · 2017: 13 · 2016: 12 · 2015: 16 · 2014: 15 · 2013: 7 · 2012: 22
- FWCI
- 2.82
- Type
- journal article
- Language
- en
- Open access
- green
- escholarship.org
- Locations
- Science (publishedVersion)
- PubMed (publishedVersion)
- eScholarship (California Digital Library) (submittedVersion)
- CaltechAUTHORS (California Institute of Technology) (submittedVersion)
- NASA STI Repository (National Aeronautics and Space Administration) (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Planetary Science and Exploration
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Keywords
- early Mars, magnetic dynamo, crustal magnetization, Tharsis volcanism, outgassing, carbon dioxide, global warming, water erosion, sediment transport, hydrothermal circulation, crustal cooling, crustal thickness, crustal deformation
- MeSH terms
- Atmosphere, Climate, Extraterrestrial Environment, Magnetics, Temperature, Water, Mars
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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