Meridiani Planum and the global hydrology of Mars

被引:0
|
作者
Jeffrey C. Andrews-Hanna
Roger J. Phillips
Maria T. Zuber
机构
[1] Washington University,McDonnell Center for the Space Sciences and the Department of Earth and Planetary Sciences
[2] St Louis,Department of Earth
[3] Missouri 63130,undefined
[4] USA,undefined
[5] Atmospheric,undefined
[6] and Planetary Sciences,undefined
[7] Massachusetts Institute of Technology,undefined
[8] Cambridge,undefined
[9] Massachusetts 02139,undefined
[10] USA,undefined
[11] Present address: Department of Earth,undefined
[12] Atmospheric,undefined
[13] and Planetary Sciences,undefined
[14] Massachusetts Institute of Technology,undefined
[15] Cambridge,undefined
[16] Massachusetts 02139,undefined
[17] USA.,undefined
来源
Nature | 2007年 / 446卷
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摘要
The evaporite deposits in the Meridiani Planum region on Mars, investigated by the Opportunity rover vehicle, have been interpreted as evidence for the presence of a fluctuating water table. But there is a problem: there is no topographic basin in this region to account for the presence of evaporates in the first place. A new hydrological modelling study circumvents this difficulty by presenting a mechanism by which evaporites could have formed at Meridiani without the need for water to collect in an enclosed basin, as a result of sustained global groundwater upwelling and evaporation.
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页码:163 / 166
页数:3
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