发现一个侧面火山口和非常年轻的冰川活动在Hecates Tholus,火星
Ernst Hauber1, Stephan van Gasselt, Boris Ivanov
1Institute of Planetary Research, German Aerospace Center (DLR), 12489 Berlin, Germany. Ernst.Hauber@dlr.de
Nature
|March 18, 2005
概括
在火星的赫卡特斯托洛斯 (Hekates Tholus) 发现了一个大型,古老的爆炸性火山爆发的证据. 这一发现,以及非常年轻的冰川沉积物,表明最近的火星气候变化与行星倾斜变化有关.
科学领域:
- 行星科学 行星科学
- 火山学 火山学是一门学科.
- 冰川学的冰川学
背景情况:
- 火星的火山活动主要是流的和巨大的.
- 爆炸性火山活动的证据很少,通常在古老的表面上发现.
研究的目的:
- 为了调查之前未知的爆炸性火山活动的痕迹在海卡特斯·托洛斯.
- 为了确定火星上的火山和冰川特征的年龄.
- 为了推断火星最近的气候变化.
主要方法:
- 分析高分辨率图像和地形数据.
- 石坑计数用于年龄的确定.
- 与气候模型进行比较.
主要成果:
- 发现了一个直径为10公里的火山口,来自于大约3.5亿年前的爆炸性喷发.
- 在火山口内确定年轻的冰川沉积物 (5-24万年).
- 冰川沉积物年龄与行星倾斜度增加的时期的相关性.
结论:
- 火星上大规模的爆炸性火山活动超越了它的早期历史.
- 年轻冰川特征的存在表明火星最近的气候变化.
- 火星的气候似乎对轴向倾斜 (斜率) 的变化敏感.
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