《火星地貌》(Martian Geomorphology)英文版[PDF]
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电驴资源
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| [火星地貌].(Martian.Geomorphology),.M.R.Balme,.A.S.Bargery,.C.J.Gallagher,.S.Gupta,.文字版.pdf | 14.11 MB |
| 14.11 MB | |
电驴资源简介
| 资源介绍 |
| 语言: 英文 |
| 地区: 英国 |
| 图书fenlei: 科技 |
| 中文名: 火星地貌 |
| 发行时间: 2011年 |
| 原名: Martian Geomorphology |
| 资源格式: PDF |
| 版本: 英文版 |
简介:  内容介绍： 火星（Mars）是太阳系八大行星之一，是太阳系由内往外数的第四颗行星，属于类地行星，直径约为地球的一半，自转轴倾角、自转周期均与地球相近，公转一周约为地球公转时间的两倍。在西方称为“战神玛尔斯”，中国则称为“荧惑”。橘红色外表是因为地表的赤铁矿（氧化铁）。火星基本上是沙漠行星，地表沙丘、砾石遍布，没有稳定的液态水体。二氧化碳为主的大气既稀薄又寒冷，沙尘悬浮其中，每年常有尘暴发生。火星两极皆有水冰与干冰组成的极冠，会随着季节消长。 内容截图： 
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目录: Preface vii Acknowledgements viii BALME, M. R., BARGERY, A. S., GALLAGHER,C. J.&GUPTA, S. Martian Geomorphology: introduction 1 BARGERY, A. S., BALME, M. R., WARNER, N., GALLAGHER,C.J.&GUPTA, S. A background to Mars exploration and research 5 MURRAY,J.B.&ILIFFE, J. C. Morphological and geographical evidence for the origin of Phobos’ grooves from HRSCMars Expressimages 21 VANGASSELT, S., HAUBER, E., ROSSI, A.-P., DUMKE, A., OROSEI,R.&NEUKUM, G. Periglacial geomorphology and landscape evolution of the Tempe Terra region, Mars 43 ROSSI, A. P., VANGASSELT, S., PONDRELLI, M., DOHM, J., HAUBER, E., DUMKE, A., ZEGERS,T.& NEUKUM, G. Evolution of periglacial landforms in the ancient mountain range of the Thaumasia Highlands, Mars 69 GALLAGHER,C.J.&BALME, M. R. Landforms indicative of ground-ice thaw in the northern high latitudes of Mars 87 HAUBER, E., REISS, D., ULRICH, M., PREUSKER, F., TRAUTHAN, F., ZANETTI, M., HIESINGER, H., JAUMANN, R., JOHANSSON, L., JOHNSSON, A., VANGASSELT,S.&OLVMO, M. Landscape evolution in Martian mid-latitude regions: insights from analogous periglacial landforms in Svalbard 111 MANGOLD, N. Water ice sublimation-related landforms on Mars 133 ASTON, A. H., CONWAY,S.J.&BALME, M. R. Identifying Martian gully evolution 151 CONWAY, S. J., BALME, M. R., MURRAY, J. B., TOWNER, M. C., OKUBO,C.H.&GRINDROD,P.M. The indication of Martian gully formation processes by slope – area analysis 171 BALME, M. R., GALLAGHER, C. J., GUPTA,S.&MURRAY, J. B. Fill and spill in Lethe Vallis: a recent flood-routing system in Elysium Planitia, Mars 203 TOWNER, M. C., EAKIN, C., CONWAY,S.J.&HARRISON, S. Geologically recent water flow inferred in channel systems in the NE Sulci Gordii region, Mars 229 KNEISSL, T., VANGASSELT, S., WENDT, L., GROSS,C.&NEUKUM, G. Layering and degradation of the Rupes Tenuis unit, Mars – a structural analysis south of Chasma Boreale 257 SOWE, M., JAUMANN,R.&NEUKUM, G. A comparative study of interior layered deposits on Mars 281 Index 301 |