Trampert jeannot (15 Ergebnisse)
Earth's Deep Mantle : Structure, Composition, And Evolution
Hilst, Robert Dirk Van Der (EDT); Bass, Jay D. (EDT); Matas, Jan (EDT); Trampert, Jeannot (EDT)
Sprache: Englisch
Verlag: American Geophysical Union, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
Anbieter: GreatBookPrices, Columbia, MD, USAGreatBookPrices
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EUR 79,00
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Earth's Deep Mantle: Structure, Composition, and Evolution, Volume 160 Format: Hardcover
Editor: Robert D. van der Hilst; Editor: Jay D. Bass (Department of Geology, University of Illinois, at Urbana-Champaign); Editor: Jan Matas; Editor: Jeannot Trampert
Sprache: Englisch
Verlag: John Wiley and Sons, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
Anbieter: INDOO, Avenel, NJ, USAINDOO
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EUR 81,50
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Zustand: New. Brand New.
Earth's Deep Mantle : Structure, Composition, And Evolution
Hilst, Robert Dirk Van Der (EDT); Bass, Jay D. (EDT); Matas, Jan (EDT); Trampert, Jeannot (EDT)
Sprache: Englisch
Verlag: American Geophysical Union, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
Anbieter: GreatBookPrices, Columbia, MD, USAGreatBookPrices
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EUR 90,94
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Zustand: As New. Unread book in perfect condition.
Sprache: Englisch
Verlag: John Wiley & Sons Inc, Wasington, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
Anbieter: Grand Eagle Retail, Bensenville, IL, USAGrand Eagle Retail
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Hardcover. Zustand: new. Hardcover. Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 160. Understanding the inner workings of our planet and its relationship to processes closer to the surface remains a frontier in the geosciences. Manmade probes barely reach 10 km depth and volcani…sm rarely brings up samples from deeper than 150 km. These distances are dwarfed by Earth's dimensions, and our knowledge of the deeper realms is pieced together from a range of surface observables, meteorite and solar atmosphere analyses, experimental and theoretical mineral physics and rock mechanics, and computer simulations. A major unresolved issue concerns the nature of mantle convection, the slow (1-5 cm/year) solid-state stirring that helps cool the planet by transporting radiogenic and primordial heat from Earth's interior to its surface. Expanding our knowledge here requires input from a range of geoscience disciplines, including seismology, geodynamics, mineral physics, and mantle petrology and chemistry. At the same time, with better data sets and faster computers, seismologists are producing more detailed models of 3-D variations in the propagation speed of different types of seismic waves; new instrumentation and access to state-of-the-art community facilities such as synchrotrons have enabled mineral physicists to measure rock and mineral properties at ever larger pressures and temperatures; new generations of mass spectrometers are allowing geo-chemists to quantify minute concentrations of diagnostic isotopes; and with supercomputers geodynamicists are making increasingly realistic simulations of dynamic processes at conditions not attainable in analogue experiments. But many questions persist. What causes the lateral variations in seismic wavespeed that we can image with mounting accuracy? How reliable are extrapolations of laboratory measurements on simple materials over many orders of magnitude of pressure and temperature? What are the effects of volatiles and minor elements on rock and mineral properties under extreme physical conditions? Can ab initio calculations help us understand material behavior in conditions that are still out of reach of laboratory measurement? What was the early evolution of our planet and to what extent does it still influence present-day dynamics? And how well do we know such first-order issues as the average bulk composition of Earth? Shipping may be from multiple locations in the US or from the UK, depending on stock availability.
Sprache: Englisch
Verlag: American Geophysical Union, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
Anbieter: Books Puddle, New York, NY, USABooks Puddle
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EUR 99,02
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Zustand: New. pp. vii + 334.
Sprache: Englisch
Verlag: American Geophysical Union, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
Anbieter: Majestic Books, Hounslow, Vereinigtes KönigreichMajestic Books
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EUR 97,68
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Zustand: New. pp. vii + 334 Illus.
Earth's Deep Mantle : Structure, Composition, And Evolution
Hilst, Robert Dirk Van Der (EDT); Bass, Jay D. (EDT); Matas, Jan (EDT); Trampert, Jeannot (EDT)
Sprache: Englisch
Verlag: American Geophysical Union, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
Anbieter: GreatBookPricesUK, Woodford Green, Vereinigtes KönigreichGreatBookPricesUK
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EUR 99,98
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Zustand: As New. Unread book in perfect condition.
Sprache: Englisch
Verlag: American Geophysical Union, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
Anbieter: Ubiquity Trade, Miami, FL, USAUbiquity Trade
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EUR 119,50
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Zustand: New. Brand new! Please provide a physical shipping address.
Earth's Deep Mantle : Structure, Composition, And Evolution
Hilst, Robert Dirk Van Der (EDT); Bass, Jay D. (EDT); Matas, Jan (EDT); Trampert, Jeannot (EDT)
Sprache: Englisch
Verlag: American Geophysical Union, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
Anbieter: GreatBookPricesUK, Woodford Green, Vereinigtes KönigreichGreatBookPricesUK
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Zustand: New.
Sprache: Englisch
Verlag: American Geophysical Union, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
Anbieter: Anybook.com, Lincoln, Vereinigtes KönigreichAnybook.com
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Zustand: Good. This is an ex-library book and may have the usual library/used-book markings inside.This book has hardback covers. In good all round condition. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,1200grams, ISBN:9780875904252.
Sprache: Englisch
Verlag: American Geophysical Union, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
- Erstausgabe
Anbieter: Kennys Bookshop and Art Galleries Ltd., Galway, GY, IrlandKennys Bookshop and Art Galleries Ltd.
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EUR 111,58
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Zustand: New. Editor(s): Van Der Hilst, Robert D; Bass, Jay D (Department of Geology, University of Illinois, at Urbana-Champaign); Matas, Jan; Trampert, Jeannot. Num Pages: 341 pages, illustrations. BIC Classification: RBG. Category: (G) General (US: Trade). Dimension: 440 x 278 x 23. Weight in Grams: 1142. . 2005. 1st Edition.… Hardcover. . . . .
Sprache: Englisch
Verlag: American Geophysical Union, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
Anbieter: Kennys Bookstore, Olney, MD, USAKennys Bookstore
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EUR 141,73
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Zustand: New. Editor(s): Van Der Hilst, Robert D; Bass, Jay D (Department of Geology, University of Illinois, at Urbana-Champaign); Matas, Jan; Trampert, Jeannot. Num Pages: 341 pages, illustrations. BIC Classification: RBG. Category: (G) General (US: Trade). Dimension: 440 x 278 x 23. Weight in Grams: 1142. . 2005. 1st Edition.… Hardcover. . . . . Books ship from the US and Ireland.
Sprache: Englisch
Verlag: John Wiley & Sons Inc, Wasington, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
Anbieter: CitiRetail, Stevenage, Vereinigtes KönigreichCitiRetail
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EUR 115,74
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Hardcover. Zustand: new. Hardcover. Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 160. Understanding the inner workings of our planet and its relationship to processes closer to the surface remains a frontier in the geosciences. Manmade probes barely reach 10 km depth and volcani…sm rarely brings up samples from deeper than 150 km. These distances are dwarfed by Earth's dimensions, and our knowledge of the deeper realms is pieced together from a range of surface observables, meteorite and solar atmosphere analyses, experimental and theoretical mineral physics and rock mechanics, and computer simulations. A major unresolved issue concerns the nature of mantle convection, the slow (1-5 cm/year) solid-state stirring that helps cool the planet by transporting radiogenic and primordial heat from Earth's interior to its surface. Expanding our knowledge here requires input from a range of geoscience disciplines, including seismology, geodynamics, mineral physics, and mantle petrology and chemistry. At the same time, with better data sets and faster computers, seismologists are producing more detailed models of 3-D variations in the propagation speed of different types of seismic waves; new instrumentation and access to state-of-the-art community facilities such as synchrotrons have enabled mineral physicists to measure rock and mineral properties at ever larger pressures and temperatures; new generations of mass spectrometers are allowing geo-chemists to quantify minute concentrations of diagnostic isotopes; and with supercomputers geodynamicists are making increasingly realistic simulations of dynamic processes at conditions not attainable in analogue experiments. But many questions persist. What causes the lateral variations in seismic wavespeed that we can image with mounting accuracy? How reliable are extrapolations of laboratory measurements on simple materials over many orders of magnitude of pressure and temperature? What are the effects of volatiles and minor elements on rock and mineral properties under extreme physical conditions? Can ab initio calculations help us understand material behavior in conditions that are still out of reach of laboratory measurement? What was the early evolution of our planet and to what extent does it still influence present-day dynamics? And how well do we know such first-order issues as the average bulk composition of Earth? Shipping may be from our UK warehouse or from our Australian or US warehouses, depending on stock availability.
Sprache: Englisch
Verlag: WILEY, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
Anbieter: moluna, Greven, Deutschlandmoluna
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EUR 111,55
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Zustand: New. KlappentextrnrnPublished by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 160. Understanding the inner workings of our planet and its relationship to processes closer to the surface remains a f.
Sprache: Englisch
Verlag: John Wiley & Sons Inc, Wasington, 2005
Serie: Geophysical Monograph, Buch 136 von 266. Buch 136 von 266 - Geophysical Monograph
- Hardcover
Anbieter: AussieBookSeller, Truganina, VIC, AustralienAussieBookSeller
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Hardcover. Zustand: new. Hardcover. Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 160. Understanding the inner workings of our planet and its relationship to processes closer to the surface remains a frontier in the geosciences. Manmade probes barely reach 10 km depth and volcani…sm rarely brings up samples from deeper than 150 km. These distances are dwarfed by Earth's dimensions, and our knowledge of the deeper realms is pieced together from a range of surface observables, meteorite and solar atmosphere analyses, experimental and theoretical mineral physics and rock mechanics, and computer simulations. A major unresolved issue concerns the nature of mantle convection, the slow (1-5 cm/year) solid-state stirring that helps cool the planet by transporting radiogenic and primordial heat from Earth's interior to its surface. Expanding our knowledge here requires input from a range of geoscience disciplines, including seismology, geodynamics, mineral physics, and mantle petrology and chemistry. At the same time, with better data sets and faster computers, seismologists are producing more detailed models of 3-D variations in the propagation speed of different types of seismic waves; new instrumentation and access to state-of-the-art community facilities such as synchrotrons have enabled mineral physicists to measure rock and mineral properties at ever larger pressures and temperatures; new generations of mass spectrometers are allowing geo-chemists to quantify minute concentrations of diagnostic isotopes; and with supercomputers geodynamicists are making increasingly realistic simulations of dynamic processes at conditions not attainable in analogue experiments. But many questions persist. What causes the lateral variations in seismic wavespeed that we can image with mounting accuracy? How reliable are extrapolations of laboratory measurements on simple materials over many orders of magnitude of pressure and temperature? What are the effects of volatiles and minor elements on rock and mineral properties under extreme physical conditions? Can ab initio calculations help us understand material behavior in conditions that are still out of reach of laboratory measurement? What was the early evolution of our planet and to what extent does it still influence present-day dynamics? And how well do we know such first-order issues as the average bulk composition of Earth? Shipping may be from our Sydney, NSW warehouse or from our UK or US warehouse, depending on stock availability.
