9780875904252 - earth's deep mantle: structure, composition, and evolution (160) (15 risultati)
Lingua: Inglese
Editore: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
Da: GreatBookPrices, Columbia, MD, U.S.A.GreatBookPrices
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 78,73
EUR 2,30 spedizioneSpedito in U.S.A.Quantità: 8 disponibili
Condizione: New.
Lingua: Inglese
Editore: John Wiley and Sons 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
Da: INDOO, Avenel, NJ, U.S.A.INDOO
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EUR 81,11
Spedizione gratuitaSpedito in U.S.A.Quantità: Più di 20 disponibili
Condizione: New.
Lingua: Inglese
Editore: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
Da: GreatBookPrices, Columbia, MD, U.S.A.GreatBookPrices
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Come nuovo
EUR 90,67
EUR 2,30 spedizioneSpedito in U.S.A.Quantità: 8 disponibili
Condizione: As New. Unread book in perfect condition.
Lingua: Inglese
Editore: John Wiley & Sons Inc, Wasington 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
Da: Grand Eagle Retail, Bensenville, IL, U.S.A.Grand Eagle Retail
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 100,52
Spedizione gratuitaSpedito in U.S.A.Quantità: 1 disponibili
Hardcover. Condizione: 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 volc…anism 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.
Lingua: Inglese
Editore: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
Da: Books Puddle, New York, NY, U.S.A.Books Puddle
Contatta il venditoreVenditore con 4 stelleCondizione: Nuovo
EUR 98,73
EUR 3,48 spedizioneSpedito in U.S.A.Quantità: 1 disponibili
Condizione: New. pp. vii + 334.
Lingua: Inglese
Editore: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
Da: Majestic Books, Hounslow, , Regno UnitoMajestic Books
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EUR 97,39
EUR 7,50 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 1 disponibili
Condizione: New. pp. vii + 334 Illus.
Lingua: Inglese
Editore: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
Da: GreatBookPricesUK, Woodford Green, Regno UnitoGreatBookPricesUK
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Come nuovo
EUR 98,01
EUR 17,30 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 1 disponibili
Condizione: As New. Unread book in perfect condition.
Lingua: Inglese
Editore: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
Da: Ubiquity Trade, Miami, FL, U.S.A.Ubiquity Trade
Contatta il venditoreVenditore con 4 stelleCondizione: Nuovo
EUR 119,15
EUR 2,61 spedizioneSpedito in U.S.A.Quantità: Più di 20 disponibili
Condizione: New. Brand new! Please provide a physical shipping address.
Lingua: Inglese
Editore: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
Da: GreatBookPricesUK, Woodford Green, Regno UnitoGreatBookPricesUK
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 102,85
EUR 17,30 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 1 disponibili
Condizione: New.
Lingua: Inglese
Editore: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
Da: Anybook.com, Lincoln, Regno UnitoAnybook.com
Contatta il venditoreVenditore con 5 stelleCondizione: Usato - Buono
EUR 85,99
EUR 36,21 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 1 disponibili
Condizione: 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.
Lingua: Inglese
Editore: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
- Prima edizione
Da: Kennys Bookshop and Art Galleries Ltd., Galway, GY, IrlandaKennys Bookshop and Art Galleries Ltd.
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 111,58
EUR 10,50 spedizioneSpedito da Irlanda a U.S.A.Quantità: 15 disponibili
Condizione: 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 Editi…on. Hardcover. . . . .
Lingua: Inglese
Editore: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
Da: Kennys Bookstore, Olney, MD, U.S.A.Kennys Bookstore
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 141,32
EUR 9,15 spedizioneSpedito in U.S.A.Quantità: 15 disponibili
Condizione: 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 Editi…on. Hardcover. . . . . Books ship from the US and Ireland.
Lingua: Inglese
Editore: John Wiley & Sons Inc, Wasington 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
Da: CitiRetail, Stevenage, Regno UnitoCitiRetail
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 114,01
EUR 42,67 spedizioneSpedito da Regno Unito a U.S.A.Quantità: 1 disponibili
Hardcover. Condizione: 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 volc…anism 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.
Lingua: Inglese
Editore: WILEY 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
Da: moluna, Greven, , Germaniamoluna
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 110,23
EUR 48,99 spedizioneSpedito da Germania a U.S.A.Quantità: Più di 20 disponibili
Condizione: 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.
Lingua: Inglese
Editore: John Wiley & Sons Inc, Wasington 2005
Serie: Geophysical Monograph, Libro 136 di 266. Libro 136 di 266 - Geophysical Monograph
- Rilegato
Da: AussieBookSeller, Truganina, VIC, AustraliaAussieBookSeller
Contatta il venditoreVenditore con 5 stelleCondizione: Nuovo
EUR 170,26
EUR 32,24 spedizioneSpedito da Australia a U.S.A.Quantità: 1 disponibili
Hardcover. Condizione: 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 volc…anism 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.
