Trampert jeannot (15 résultats)
Langue : anglais
Edité par American Geophysical Union 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
Vendeur : GreatBookPrices, Columbia, MD, Etats-UnisGreatBookPrices
Contacter le vendeurVendeur avec une évaluation de 5 étoilesEtat: Neuf
EUR 78,52
EUR 2,29 expéditionExpédition nationale : Etats-UnisQuantité disponible : 8 disponible(s)
Etat : New.
Langue : anglais
Edité par John Wiley and Sons 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
Vendeur : INDOO, Avenel, NJ, Etats-UnisINDOO
Contacter le vendeurVendeur avec une évaluation de 5 étoilesEtat: Neuf
EUR 80,89
Frais de port gratuitsExpédition nationale : Etats-UnisQuantité disponible : Plus de 20 disponibles
Etat : New.
Langue : anglais
Edité par American Geophysical Union 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
Vendeur : GreatBookPrices, Columbia, MD, Etats-UnisGreatBookPrices
Contacter le vendeurVendeur avec une évaluation de 5 étoilesEtat: Occasion - Comme neuf
EUR 90,43
EUR 2,29 expéditionExpédition nationale : Etats-UnisQuantité disponible : 8 disponible(s)
Etat : As New. Unread book in perfect condition.
Langue : anglais
Edité par John Wiley & Sons Inc, Wasington 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
Vendeur : Grand Eagle Retail, Bensenville, IL, Etats-UnisGrand Eagle Retail
Contacter le vendeurVendeur avec une évaluation de 5 étoilesEtat: Neuf
EUR 100,25
Frais de port gratuitsExpédition nationale : Etats-UnisQuantité disponible : 1 disponible(s)
Hardcover. Etat : 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 volcanism… 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.
Langue : anglais
Edité par American Geophysical Union 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
Vendeur : Books Puddle, New York, NY, Etats-UnisBooks Puddle
Contacter le vendeurVendeur avec une évaluation de 4 étoilesEtat: Neuf
EUR 98,47
EUR 3,47 expéditionExpédition nationale : Etats-UnisQuantité disponible : 1 disponible(s)
Etat : New. pp. vii + 334.
Langue : anglais
Edité par American Geophysical Union 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
Vendeur : Majestic Books, Hounslow, , Royaume-UniMajestic Books
Contacter le vendeurVendeur avec une évaluation de 4 étoilesEtat: Neuf
EUR 97,13
EUR 7,51 expéditionExpédition depuis Royaume-Uni vers Etats-UnisQuantité disponible : 1 disponible(s)
Etat : New. pp. vii + 334 Illus.
Langue : anglais
Edité par American Geophysical Union 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
Vendeur : GreatBookPricesUK, Woodford Green, Royaume-UniGreatBookPricesUK
Contacter le vendeurVendeur avec une évaluation de 5 étoilesEtat: Occasion - Comme neuf
EUR 98,24
EUR 17,34 expéditionExpédition depuis Royaume-Uni vers Etats-UnisQuantité disponible : 1 disponible(s)
Etat : As New. Unread book in perfect condition.
Langue : anglais
Edité par American Geophysical Union 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
Vendeur : Ubiquity Trade, Miami, FL, Etats-UnisUbiquity Trade
Contacter le vendeurVendeur avec une évaluation de 4 étoilesEtat: Neuf
EUR 118,83
EUR 2,61 expéditionExpédition nationale : Etats-UnisQuantité disponible : Plus de 20 disponibles
Etat : New. Brand new! Please provide a physical shipping address.
Langue : anglais
Edité par American Geophysical Union 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
Vendeur : GreatBookPricesUK, Woodford Green, Royaume-UniGreatBookPricesUK
Contacter le vendeurVendeur avec une évaluation de 5 étoilesEtat: Neuf
EUR 103,09
EUR 17,34 expéditionExpédition depuis Royaume-Uni vers Etats-UnisQuantité disponible : 1 disponible(s)
Etat : New.
Langue : anglais
Edité par American Geophysical Union 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
Vendeur : Anybook.com, Lincoln, Royaume-UniAnybook.com
Contacter le vendeurVendeur avec une évaluation de 5 étoilesEtat: Occasion - Satisfaisant
EUR 86,19
EUR 36,29 expéditionExpédition depuis Royaume-Uni vers Etats-UnisQuantité disponible : 1 disponible(s)
Etat : 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.
Langue : anglais
Edité par American Geophysical Union 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
- Édition originale
Vendeur : Kennys Bookshop and Art Galleries Ltd., Galway, GY, IrlandeKennys Bookshop and Art Galleries Ltd.
Contacter le vendeurVendeur avec une évaluation de 5 étoilesEtat: Neuf
EUR 111,58
EUR 10,50 expéditionExpédition depuis Irlande vers Etats-UnisQuantité disponible : 15 disponible(s)
Etat : 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. H…ardcover. . . . .
Langue : anglais
Edité par American Geophysical Union 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
Vendeur : Kennys Bookstore, Olney, MD, Etats-UnisKennys Bookstore
Contacter le vendeurVendeur avec une évaluation de 5 étoilesEtat: Neuf
EUR 140,94
EUR 9,13 expéditionExpédition nationale : Etats-UnisQuantité disponible : 15 disponible(s)
Etat : 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. H…ardcover. . . . . Books ship from the US and Ireland.
Langue : anglais
Edité par John Wiley & Sons Inc, Wasington 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
Vendeur : CitiRetail, Stevenage, Royaume-UniCitiRetail
Contacter le vendeurVendeur avec une évaluation de 5 étoilesEtat: Neuf
EUR 114,28
EUR 42,77 expéditionExpédition depuis Royaume-Uni vers Etats-UnisQuantité disponible : 1 disponible(s)
Hardcover. Etat : 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 volcanism… 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.
Langue : anglais
Edité par WILEY 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
Vendeur : moluna, Greven, , Allemagnemoluna
Contacter le vendeurVendeur avec une évaluation de 5 étoilesEtat: Neuf
EUR 110,23
EUR 48,99 expéditionExpédition depuis Allemagne vers Etats-UnisQuantité disponible : Plus de 20 disponibles
Etat : 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.
Langue : anglais
Edité par John Wiley & Sons Inc, Wasington 2005
Série : Geophysical Monograph, Livre 136 sur 266. Livre 136 sur 266 - Geophysical Monograph
- Couverture rigide
Vendeur : AussieBookSeller, Truganina, VIC, AustralieAussieBookSeller
Contacter le vendeurVendeur avec une évaluation de 5 étoilesEtat: Neuf
EUR 170,01
EUR 32,16 expéditionExpédition depuis Australie vers Etats-UnisQuantité disponible : 1 disponible(s)
Hardcover. Etat : 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 volcanism… 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.
