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DOI | 10.1126/science.1101812 |
New perspectives on ancient Mars | |
Solomon S.C.; Aharonson O.; Aurnou J.M.; Banerdt W.B.; Carr M.H.; Dombard A.J.; Frey H.V.; Golombek M.P.; Hauck II S.A.; Head III J.W.; Jakosky B.H.; Johnson C.L.; McGovern P.J.; Neumann G.A.; Phillips R.J.; Smith D.E.; Zuber M.T. | |
发表日期 | 2005 |
ISSN | 0036-8075 |
起始页码 | 1214 |
结束页码 | 1220 |
卷号 | 307期号:5713 |
英文摘要 | Mars was most active during its first billion years. The core, mantle, and crust formed within ∼50 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. |
英文关键词 | Carbon dioxide; Climate change; Cooling; Earth atmosphere; Erosion; Magnetization; Martian surface analysis; Sediment transport; Solar system; Water; Wind; Climate warming; Crustal magnetization; Magnetic dynamo; Solar wind; Planets; carbon dioxide; water; core (planetary); crust; mantle; Mars; planetary evolution; volcanism; astronomy; atmosphere; climate change; magnetism; priority journal; review; sediment transport; sedimentation; solar energy; warming; wind; Atmosphere; Climate; Extraterrestrial Environment; Magnetics; Mars; Temperature; Water |
语种 | 英语 |
来源期刊 | Science
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/245554 |
作者单位 | Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC 20015, United States; Div. of Geol. and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, United States; Dept. of Earth and Space Sciences, University of California, Los Angeles, CA 90095, United States; Jet Propulsion Laboratory, Pasadena, CA 91109, United States; U.S. Geological Survey, Menlo Park, CA 94025, United States; Dept. of Earth and Planet. Sciences, Washington University, St. Louis, MO 63130, United States; Laboratory for Terrestrial Physics, NASA Goddard Space Flight Center, Greenbelt, MD 20771, United States; Department of Geological Sciences, Case Western Reserve University, Cleveland, OH 44106, United States; Department of Geological Sciences, Brown University, Providence, RI 02912, United States; Lab. for Atmosph. and Space Physics, Department of Geological Sciences, University of Colorado, Boulder, CO 80309, United States; Inst. of Geophys. and Planet. Phys., Scripps Institut... |
推荐引用方式 GB/T 7714 | Solomon S.C.,Aharonson O.,Aurnou J.M.,et al. New perspectives on ancient Mars[J],2005,307(5713). |
APA | Solomon S.C..,Aharonson O..,Aurnou J.M..,Banerdt W.B..,Carr M.H..,...&Zuber M.T..(2005).New perspectives on ancient Mars.Science,307(5713). |
MLA | Solomon S.C.,et al."New perspectives on ancient Mars".Science 307.5713(2005). |
条目包含的文件 | 条目无相关文件。 |
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