Martian aeolian geomorphology : an introduction / Zhibao Dong, Chao Li, Ping Lü
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| Autore: | Dong, Zhibao |
| Titolo: | Martian aeolian geomorphology : an introduction / Zhibao Dong, Chao Li, Ping Lü |
| Pubblicazione: | Cham, : Springer, 2025 |
| Descrizione fisica: | 1 testo elettronico (XIX, 570 p. : ill.) |
| Disciplina: | 910.02(Geografia fisica) |
| 551(Geologia, idrogeologia, meteorologia) | |
| 551.41(Geomorfologia) | |
| 523.1(Cosmologia) | |
| 523.01(Astrofisica) | |
| 520(Astronomia) | |
| Soggetto non controllato: | Aeolian Geomorphology |
| Geomorphology | |
| Martian Aeolian Geomorphology | |
| Martian Geomorphology | |
| Martian Science | |
| Planetary Aeolian Geomorphology | |
| Planetary Geomorphology | |
| Planetary science | |
| Altri autori: | Li, Chao Lü, Ping |
| Sommario/riassunto: | This book covers Martian Aeolian Geomorphology and is organized around three main foci. The first focus is about advancing our understanding of aeolian geomorphology through research on Martian aeolian landforms. Chapters 1 through 4 provide essential knowledge for understanding the aeolian geomorphology of Mars. Among them, Chapters 1 and 2 provide readers with a clear understanding of the significance, scientific status and methodology of the study of aeolian geomorphology on Mars. Chapters 3 introduces the physics of aeolian geomorphology and Chapter 4 presents an overview of Mars. Chapters 5 and 6 are devoted to the Martian atmosphere, and Martian sediments respectively, constituting the dynamic conditions and the material basis for the formation of aeolian landforms, their basic characteristics, the processes that control their formation and evolution, and comparisons with Earth. (Estratto dal sito dell'editore) |
| Formato: | Materiale a stampa  |
| Livello bibliografico | Monografia |
| Lingua di pubblicazione: | Inglese |
| Record Nr.: | VAN00309015 |
| Lo trovi qui: | Univ. Vanvitelli |
| Localizzazioni e accesso elettronico | https://doi.org/10.1007/978-3-031-83848-4 |
| Opac: | Controlla la disponibilità qui |