西部Valles Marineris轻调分层沉积物和新分类的边缘沉积物的地图绘制
Ivan G Mishev1, Isaac B Smith1,2, Cathy Quantin3
1York University Toronto ON Canada.
概括
新的雷达和图像数据显示,在Valles Marineris附近有三种类型的火星边缘沉积物. 这些浅色层层沉积物 (LLDs),弱层层沉积物 (WLDs) 和无层层沉积物 (NDs) 可能是由水改变的火山灰形成的.
科学领域:
- 行星科学 行星科学
- 火山学 火山学是一门学科.
- 地质地质地质地质地质地
背景情况:
- 分层沉积物,称为浅色分层沉积物 (LLDs),围绕着火星上的Valles Marineris.
- 据信,LLDs是火山火灰,经过化学过程而改变.
研究的目的:
- 确定和绘制Valles Marineris附近不同类型的边缘沉积物的地图.
- 调查这些沉积物的起源和改造过程.
主要方法:
- 浅层雷达 (SHARAD) 用于检测沉积物底部的雷达反射.
- 高分辨率成像科学实验 (HiRISE),上下文摄像机 (CTX) 和火星观测摄像机 (MOC-NA) 的图像被用于绘制地图.
- 对边缘沉积物的全部范围进行了地质测绘.
主要成果:
- 确定了三种类型的边缘沉积物:浅色层沉积物 (LLD),弱层沉积物 (WLD) 和无层沉积物 (ND).
- WLDs和NDs与LLDs相邻,这表明它们有共同的起源.
- 创建了所有边缘沉积物的全面地图.
结论:
- 这三种类型的沉积物都可能起源于火相的灰.
- 层次的变化表明液态水的不同程度的修饰.
- 潜在的火山源包括Tharsis火山和Noctis Labyrinthus中一个假设的火山,研究了过去水环境的证据.
关键词:
莎拉德·沙拉德 (Sharad Sharad) 是一个著名的作家.瓦莱斯·马里内里斯 (Valles Marineris) 是一个海上山谷.层层的沉积物是层层的沉积物.诺克蒂斯·诺克蒂斯 (英语:Noctis noctis) 是一个夜晚的生物.雷达 雷达 雷达 雷达 是一个火山火山火山火山火山火山火山火山火山更多相关视频
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