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Overview of the Mars Pathfinder mission and assessment of landing site predictions

机译:火星探路者任务概述和着陆点预测评估

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Chemical analyses returned by Mars Pathfinder indicate that some rocks may be high in silica, implying differentiated parent materials. Rounded pebbles and cobbles and a possible conglomerate suggest fluvial processes that imply liquid water in equilibrium with the atmosphere and thus a warmer and wetter past. The moment of inertia indicates a central metallic core of 1300 to 2000 kilometers in radius. Composite airborne dust particles appear magnetized by freeze-dried maghemite stain or cement that may have been leached from crustal materials by an active hydrologic cycle. Remote-sensing data at a scale of generally greater than approximately 1 kilometer and an Earth analog correctly predicted a rocky plain safe for landing and roving with a variety of rocks deposited by catastrophic floods that are relatively dust-free.
机译:火星探路者(Mars Pathfinder)返回的化学分析表明,某些岩石中的二氧化硅含量可能很高,这意味着母体材料有所不同。圆形的鹅卵石和鹅卵石以及可能的砾岩暗示了河流形成的过程,这意味着液态水与大气处于平衡状态,因此过去温暖潮湿。惯性矩表示中心金属核的半径为1300至2000公里。空气中的复合尘埃颗粒似乎被冻干的磁赤铁矿污渍或水泥所磁化,这些物质可能是通过活跃的水文循环从地壳材料中浸出的。遥感数据的规模通常大于大约1公里,并且地球类似物正确地预测了岩石着陆的安全性,可以用相对无尘的灾难性洪水沉积的各种岩石来着陆和巡回。

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