Anthony dosseto (3 Ergebnisse)
Timescales of Magmatic Processes From Core to Atmosphere
Dosseto, Anthony; Tuner, Simon P. and Van Orman, James A. (Eds)
- Hardcover
- Erstausgabe
Anbieter: Peter Rhodes, Southampton, Vereinigtes KönigreichPeter Rhodes
Verkäufer/-in kontaktierenVerkäufer/-in mit 4 SternenZustand: Gebraucht - Gut
EUR 32,56
EUR 41,81 VersandVersand von Vereinigtes Königreich nach USAAnzahl: 1 verfügbar
Hard Cover. Zustand: Very Good. First Hardback Edition. 255 x 195mm. pp. 264. English text. First hardback edition of 'Timescales of Magmatic Processes from Core to Atmosphere'. Colour and black and white illustrations. Bound in original pictorial baords. No dust jacket [as published]. A few very light bumps and marks, otherwise… clean. Binding strong. No ownership inscription or underlining. See images.
- Softcover
Anbieter: Phatpocket Limited, Waltham Abbey, HERTS, Vereinigtes KönigreichPhatpocket Limited
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EUR 62,97
EUR 12,46 VersandVersand von Vereinigtes Königreich nach USAAnzahl: 1 verfügbar
Zustand: Good. Your purchase helps support Sri Lankan Children's Charity 'The Rainbow Centre'. Ex-library, so some stamps and wear, but in good overall condition. Our donations to The Rainbow Centre have helped provide an education and a safe haven to hundreds of children who live in appalling conditions.
- Weitere Bilder
- Softcover
Anbieter: Optimon Books, Gravesend, KENT, Vereinigtes KönigreichOptimon Books
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EUR 67,53
EUR 21,08 VersandVersand von Vereinigtes Königreich nach USAAnzahl: 1 verfügbar
Paperback. Zustand: Good. Quantifying the timescales of current geological processes is critical for constraining the physical mechanisms operating on the Earth today. Since the Earth's origin 4.55 billion years ago magmatic processes have continued to shape the Earth, producing the major reservoirs that exist today (core, mantl…e, crust, oceans and atmosphere) and promoting their continued evolution. But key questions remain. When did the core form and how quickly? How are magmas produced in the mantle, and how rapidly do they travel towards the surface? How long do magmas reside in the crust, differentiating and interacting with the host rocks to yield the diverse set of igneous rocks we see today? How fast are volc.
