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达丽深谷

达丽狄安娜峡谷(英语:Dali and Diana Chasma)组成的深谷系统长达7400公里,是金星上非常突出的地形特征。这些峡谷通过雅特拉区的大型火山连接到奥瓦达区和忒提斯区高原,因而被认为是阿佛洛狄忒高地的“蝎子尾巴”。广阔、弯曲的陡坡类似地球上压入另一地壳下的板块俯冲带。沿峡谷最高处边缘,高亮的雷达信号反映,与其它较高原地区类似,其表面可能存在一些如黄铁矿的金属矿物。[1]

参考资料

[编辑]
  1. ^ Catalog Page for PIA00268. [2014-01-15]. (原始内容存档于2021-03-18). 
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达丽深谷
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