首页> 外文会议>55th International Astronautical Congress 2004 vol.10 >THE SURFACE OF ICE AS (CRYO)GEOLOGIC LANDFORM - LANDFORM TYPES OF TERRESTRIAL LAKE ICE AND THE SURFACE OF EUROPA
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THE SURFACE OF ICE AS (CRYO)GEOLOGIC LANDFORM - LANDFORM TYPES OF TERRESTRIAL LAKE ICE AND THE SURFACE OF EUROPA

机译:冰(CRYO)地质地貌的面-陆地湖冰的地貌类型和欧罗巴的面

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摘要

Ice features of lake ice on Earth and the ice cover of Europa can be viewed both as hidrologic feature, or as cryogeologic feature. Both can be used for determining terrestrial paleolandscapes of ice ages. Water can be considered as a one component magma, where "thermal differentiation" (or simple surficial cooling) creates its crust instead of chemical differentiation. Lake ice is considered as a miniature natural lab of cryo- and normal geological features and processes.
机译:地球上的湖泊冰层和欧罗巴的冰盖的冰层特征既可以看作是水文特征,也可以看作是低温地质特征。两者都可用于确定冰河时代的陆地古地貌。水可以被认为是一种岩浆成分,其中“热分异”(或简单的表面冷却)产生了其地壳而不是化学分异。湖冰被认为是具有低温和正常地质特征及过程的微型天然实验室。

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