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DOI10.1126/science.1058701
Ancient geodynamics and global-scale hydrology on Mars
Phillips R.J.; Zuber M.T.; Solomon S.C.; Golombek M.P.; Jakosky B.M.; Banerdt W.B.; Smith D.E.; Williams R.M.E.; Hynek B.M.; Aharonson O.; Hauck II S.A.
发表日期2001
ISSN0036-8075
起始页码2587
结束页码2591
卷号291期号:5513
英文摘要Loading of the lithosphere of Mars by the Tharsis rise explains much of the global shape and long-wavelength gravity field of the planet, including a ring of negative gravity anomalies and a topographic trough around Tharsis, as well as gravity anomaly and topographic highs centered in Arabia Terra and extending northward toward Utopia. The Tharsis-induced trough and antipodal high were largely in place by the end of the Noachian Epoch and exerted control on the location and orientation of valley networks. The release of carbon dioxide and water accompanying the emplacement of ∼3 × 108 cubic kilometers of Tharsis magmas may have sustained a warmer climate than at present, enabling the formation of ancient valley networks and fluvial landscape denudation in and adjacent to the large-scale trough.
英文关键词Carbon dioxide; Gravitation; Water; Fluvial landscape denudation; Topographic high; Hydrogeology; article; astronomy; evolution; geology; gravity; model; priority journal; space; three dimensional imaging; Atmosphere; Carbon Dioxide; Evolution, Planetary; Extraterrestrial Environment; Gravitation; Mars; Water
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/245078
作者单位McDonnell Ctr. for the Space Sci., Dept. of Earth/Planetary Sciences, Washington University, St. Louis, MO 63130, United States
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Phillips R.J.,Zuber M.T.,Solomon S.C.,et al. Ancient geodynamics and global-scale hydrology on Mars[J],2001,291(5513).
APA Phillips R.J..,Zuber M.T..,Solomon S.C..,Golombek M.P..,Jakosky B.M..,...&Hauck II S.A..(2001).Ancient geodynamics and global-scale hydrology on Mars.Science,291(5513).
MLA Phillips R.J.,et al."Ancient geodynamics and global-scale hydrology on Mars".Science 291.5513(2001).
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