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机译:水星从复杂的火山口到峰环盆地的过渡:MESSENGER飞越数据的新观察和盆地形成模型的约束
Department of Geological Sciences, Brown University, Box 1846, Providence, Rl 02912, USA;
Department of Geological Sciences, Brown University, Box 1846, Providence, Rl 02912, USA;
Department of Geological Sciences, Brown University, Box 1846, Providence, Rl 02912, USA;
Johns Hopkins University Applied Physics Laboratory, 11100 Johns Hopkins Road, Laurel, MD 20723, USA;
Johns Hopkins University Applied Physics Laboratory, 11100 Johns Hopkins Road, Laurel, MD 20723, USA;
Johns Hopkins University Applied Physics Laboratory, 11100 Johns Hopkins Road, Laurel, MD 20723, USA;
Johns Hopkins University Applied Physics Laboratory, 11100 Johns Hopkins Road, Laurel, MD 20723, USA;
Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC 20015, USA;
Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721, USA;
mercury; peak ring; impact process; crater; basin; MESSENGER;
机译:来自MESSENGER和LRO测高仪的水星和月球陨石坑和盆地的新形态测量和图像数据:用于评估峰环盆地形成模型的观测框架
机译:从复合火山口过渡到月球上的峰环盆地的转换的奉承重力观测:用于地壳结构和冲击盆地形成的影响
机译:Eminescu的撞击结构:洞察从复杂的火山口向水星上的峰环盆地过渡
机译:汞多环盆地的火山口检测
机译:泥盆纪Southesk-Cairn碳酸盐复合体(阿尔伯塔盆地)晚期成岩方解石的特征:岩石学,稳定和放射性同位素,流体包裹体和有机物成熟度数据的限制。
机译:通过数据同化将遥感信息集成到分布式水文模型中以改善大型流域的水预算预测
机译:峰环盆地的形成:使用观测来约束冲击盆地形成模型的工作假设和前进路径