9780875904252 - earth's deep mantle: structure, composition, and evolution: 160 (geophysical monograph series) (15 resultados)
Earth's Deep Mantle : Structure, Composition, And Evolution
Hilst, Robert Dirk Van Der (EDT); Bass, Jay D. (EDT); Matas, Jan (EDT); Trampert, Jeannot (EDT)
Idioma: Inglés
Editorial: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
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Librería: GreatBookPrices, Columbia, MD, Estados Unidos de AmericaGreatBookPrices
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EUR 78,85
Envío por EUR 2,30Se envía dentro de Estados Unidos de AmericaCantidad disponible: 8 disponibles
Condición: New.
Idioma: Inglés
Editorial: John Wiley and Sons 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
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Librería: INDOO, Avenel, NJ, Estados Unidos de AmericaINDOO
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EUR 81,24
Gastos de envío gratisSe envía dentro de Estados Unidos de AmericaCantidad disponible: Más de 20 disponibles
Condición: 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)
Idioma: Inglés
Editorial: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
- Tapa dura
Librería: GreatBookPrices, Columbia, MD, Estados Unidos de AmericaGreatBookPrices
Contactar con el vendedorVendedor de 5 estrellasCondición: Usado - Como Nuevo
EUR 90,81
Envío por EUR 2,30Se envía dentro de Estados Unidos de AmericaCantidad disponible: 8 disponibles
Condición: As New. Unread book in perfect condition.
Idioma: Inglés
Editorial: John Wiley & Sons Inc, Wasington 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
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Librería: Grand Eagle Retail, Bensenville, IL, Estados Unidos de AmericaGrand Eagle Retail
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EUR 100,67
Gastos de envío gratisSe envía dentro de Estados Unidos de AmericaCantidad disponible: 1 disponibles
Hardcover. Condición: 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 volca…nism 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.
Idioma: Inglés
Editorial: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
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Librería: Books Puddle, New York, NY, Estados Unidos de AmericaBooks Puddle
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EUR 98,88
Envío por EUR 3,48Se envía dentro de Estados Unidos de AmericaCantidad disponible: 1 disponibles
Condición: New. pp. vii + 334.
Idioma: Inglés
Editorial: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
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Librería: Majestic Books, Hounslow, , Reino UnidoMajestic Books
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EUR 97,54
Envío por EUR 7,49Se envía de Reino Unido a Estados Unidos de AmericaCantidad disponible: 1 disponibles
Condición: 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)
Idioma: Inglés
Editorial: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
- Tapa dura
Librería: GreatBookPricesUK, Woodford Green, Reino UnidoGreatBookPricesUK
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EUR 97,92
Envío por EUR 17,28Se envía de Reino Unido a Estados Unidos de AmericaCantidad disponible: 1 disponibles
Condición: As New. Unread book in perfect condition.
Idioma: Inglés
Editorial: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
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Librería: Ubiquity Trade, Miami, FL, Estados Unidos de AmericaUbiquity Trade
Contactar con el vendedorVendedor de 4 estrellasCondición: Nuevo
EUR 119,33
Envío por EUR 2,62Se envía dentro de Estados Unidos de AmericaCantidad disponible: Más de 20 disponibles
Condición: 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)
Idioma: Inglés
Editorial: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
- Tapa dura
Librería: GreatBookPricesUK, Woodford Green, Reino UnidoGreatBookPricesUK
Contactar con el vendedorVendedor de 5 estrellasCondición: Nuevo
EUR 102,76
Envío por EUR 17,28Se envía de Reino Unido a Estados Unidos de AmericaCantidad disponible: 1 disponibles
Condición: New.
Idioma: Inglés
Editorial: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
- Tapa dura
Librería: Anybook.com, Lincoln, Reino UnidoAnybook.com
Contactar con el vendedorVendedor de 5 estrellasCondición: Usado - Aceptable
EUR 85,92
Envío por EUR 36,18Se envía de Reino Unido a Estados Unidos de AmericaCantidad disponible: 1 disponibles
Condición: 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.
Idioma: Inglés
Editorial: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
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- Primera edición
Librería: Kennys Bookshop and Art Galleries Ltd., Galway, GY, IrlandaKennys Bookshop and Art Galleries Ltd.
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EUR 111,58
Envío por EUR 10,50Se envía de Irlanda a Estados Unidos de AmericaCantidad disponible: 15 disponibles
Condición: 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 Editio…n. Hardcover. . . . .
Idioma: Inglés
Editorial: American Geophysical Union 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
- Tapa dura
Librería: Kennys Bookstore, Olney, MD, Estados Unidos de AmericaKennys Bookstore
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EUR 141,53
Envío por EUR 9,16Se envía dentro de Estados Unidos de AmericaCantidad disponible: 15 disponibles
Condición: 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 Editio…n. Hardcover. . . . . Books ship from the US and Ireland.
Idioma: Inglés
Editorial: John Wiley & Sons Inc, Wasington 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
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Librería: CitiRetail, Stevenage, Reino UnidoCitiRetail
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EUR 113,91
Envío por EUR 42,63Se envía de Reino Unido a Estados Unidos de AmericaCantidad disponible: 1 disponibles
Hardcover. Condición: 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 volca…nism 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.
Idioma: Inglés
Editorial: WILEY 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
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Librería: moluna, Greven, , Alemaniamoluna
Contactar con el vendedorVendedor de 5 estrellasCondición: Nuevo
EUR 110,23
Envío por EUR 48,99Se envía de Alemania a Estados Unidos de AmericaCantidad disponible: Más de 20 disponibles
Condición: 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.
Idioma: Inglés
Editorial: John Wiley & Sons Inc, Wasington 2005
Serie: Geophysical Monograph, Libro 136 de 266. Libro 136 de 266 - Geophysical Monograph
- Tapa dura
Librería: AussieBookSeller, Truganina, VIC, AustraliaAussieBookSeller
Contactar con el vendedorVendedor de 5 estrellasCondición: Nuevo
EUR 170,60
Envío por EUR 32,29Se envía de Australia a Estados Unidos de AmericaCantidad disponible: 1 disponibles
Hardcover. Condición: 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 volca…nism 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.
