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Landforms on Asteroid 25143-Itokawa: A geomorphological perspective on periglacial origin and meltwater history

机译:小行星25143-Itokawa上的地貌:冰缘起源和融水历史的地貌学观点

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摘要

Asteroid surface geology offers a full range of opportunities for geomorphologists to participate in the analysis of landform distributions, deposit composition, source areas for sediments, age estimations, and the reconstruction of geohydrological records. A recent touchdown (2005) on 25143-Itokawa, a Near Earth Object (NEO), by the Hayabusa Spacecraft provides imagery (released, 2008, by the Japanese Aerospace Agency) that allows the analysis of data relevant to geomorphologists. The abbreviated interpretation of landform distributions on Itokawa discussed below provides a preliminary analysis of landform morphogenesis in a cold climate with near-zero gravity. The analysis generates several questions related to source of water, cause of fluid propagation and explanations of previously unrecognized processes of denudation.
机译:小行星表面地质学为地貌学家提供了广泛的机会,使其可以参与地貌分布,沉积物成分,沉积物来源区域,年龄估算以及地质水文记录的重建分析。 ab鸟太空船对25143-Itokawa(近地物体)的最近触地得分(2005年),提供了影像(由日本航空航天局于2008年发布),用于分析与地貌学家有关的数据。下文讨论的伊藤川地貌分布的缩写解释提供了对重力接近零的寒冷气候中地貌形态发生的初步分析。该分析产生了与水源,流体传播的原因以及先前无法识别的剥蚀过程有关的几个问题。

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