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Añadir al carritoHardcover. Condición: Fair. No Jacket. Readable copy. Pages may have considerable notes/highlighting. ~ ThriftBooks: Read More, Spend Less.
Publicado por Geological Society / Blackwell Scientific, Oxford, 1981
Librería: Victoria Bookshop, BERE ALSTON, DEVON, Reino Unido
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Añadir al carritoPaperback. Condición: Good. First Thus. 8vo c140 pp. A good copy with some minor yellowing, shelf wear and a few pressure marks to covers incl crease to spine tail corner of covers and throughout journal. articles incl: Magma accumulation in the ascending mantle. Book.
Publicado por Springer, Berlin, 1979
ISBN 10: 3540094105 ISBN 13: 9783540094104
Librería: Mike's Library LLC, Plymouth, PA, Estados Unidos de America
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Añadir al carritoHardcover. Condición: Very Good-. Estado de la sobrecubierta: No Dust Jacket. Library stamps/marks/labels/pocket, 1" tear to spine edge, otherwise light wear.; Rest of contents of Vol 85: Genetics of immunoresposiveness to natural antigens in the mouse / G. Biozzi . [et al.]; Chemistry and biology of the enterobacterial common antigen / H. Mayer, G. Schmidt; Cumulative Author and Subject Index, Volumes 40-85. ; Current Topics In Microbiology And Immunology, Vol 85; Ex-Library; Vol. 85; 184 pages.
Librería: Romtrade Corp., STERLING HEIGHTS, MI, Estados Unidos de America
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Añadir al carritoCondición: New. pp. 392.
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Añadir al carritoPaperback. Condición: Brand New. 374 pages. 9.25x6.75x0.75 inches. In Stock.
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Idioma: Inglés
Publicado por Springer Berlin Heidelberg, 2012
ISBN 10: 3642493564 ISBN 13: 9783642493560
Librería: moluna, Greven, Alemania
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Publicado por Springer Nature (Sie), 2020
Librería: Books in my Basket, New Delhi, India
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Añadir al carritoN.A. Condición: New. ISBN:9783662600542.
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Publicado por Springer Berlin Heidelberg, 2012
ISBN 10: 3642493564 ISBN 13: 9783642493560
Librería: AHA-BUCH GmbH, Einbeck, Alemania
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Añadir al carritoTaschenbuch. Condición: Neu. Druck auf Anfrage Neuware - Printed after ordering - Igneous petrology was to some extent essentially a descriptive sci ence until about 1960. The results were mainly obtained from field work, major element analyses, and microscopical studies. During the 1960's two simultaneous developments took place, plate tectonics became generally accepted, and the generation of magmas could now be related to the geodynamic features like convection cells and subduction zones. The other new feature was the development of new analytical apparatus which allowed high accuracy analyses of trace elements and isotopes. In addition it became possible to do ex perimental studies at pressures up to 100 kbar. During the 1970's a large amount of analytical data was obtained and it became evident that the igneous processes that control the compositions of magmas are not that simple to determine. The composition of a magma is controlled by the compositions of its source, the degree of partial melting, and the degree of fractionation. In order to understand the significance of these various processes the relationship between the physical processes and their geochemical consequences should be known. Presently there are several theories that attempt to explain the origin of the various magma types, and these theories can only be evaluated by turning the different ideas into quantitative models. We will so to speak have to do some book keeping for the various theories in order to see which ones are valid. the present book is intended as an introduction to the more fun damental aspects of quantitative igneous petrology.
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Añadir al carritoCondición: Sehr gut. Zustand: Sehr gut | Seiten: 390 | Sprache: Englisch | Produktart: Bücher | Keine Beschreibung verfügbar.
Librería: Ria Christie Collections, Uxbridge, Reino Unido
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Librería: Ria Christie Collections, Uxbridge, Reino Unido
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Librería: Ria Christie Collections, Uxbridge, Reino Unido
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Librería: Ria Christie Collections, Uxbridge, Reino Unido
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Publicado por Springer Berlin Heidelberg, 1985
ISBN 10: 3662600544 ISBN 13: 9783662600542
Librería: Mispah books, Redhill, SURRE, Reino Unido
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Añadir al carritoPaperback. Condición: Very Good. Dust Jacket may NOT BE INCLUDED.CDs may be missing. SHIPS FROM MULTIPLE LOCATIONS. book.
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Añadir al carritoHardcover. Condición: Very Good. Dust Jacket may NOT BE INCLUDED.CDs may be missing. SHIPS FROM MULTIPLE LOCATIONS. book.
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Añadir al carritoPaperback. Condición: Brand New. reprint edition. 148 pages. 9.50x6.60x0.40 inches. In Stock.
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Añadir al carritoPaperback. Condición: Brand New. reprint edition. 184 pages. 9.30x6.70x0.50 inches. In Stock.
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Publicado por Springer Berlin Heidelberg, 2011
ISBN 10: 3642673244 ISBN 13: 9783642673245
Librería: moluna, Greven, Alemania
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Publicado por Springer Berlin Heidelberg, 2011
ISBN 10: 3642677193 ISBN 13: 9783642677199
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Añadir al carritoCondición: New. Genetic Analysis of the lac Repressor.- Cotranslational and Posttranslational Processing of Viral Glycoproteins.- Immunity and Repression in Bacteriophages P1 and P7.- Immunochemistry of Herpes Simplex Virus Glycoproteins.- Infectious Bursal Disease Virus.-.
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Añadir al carritoCondición: new. Questo è un articolo print on demand.
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Publicado por Springer Berlin Heidelberg Apr 2012, 2012
ISBN 10: 3642493564 ISBN 13: 9783642493560
Librería: BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, Alemania
EUR 53,49
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Añadir al carritoTaschenbuch. Condición: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Igneous petrology was to some extent essentially a descriptive sci ence until about 1960. The results were mainly obtained from field work, major element analyses, and microscopical studies. During the 1960's two simultaneous developments took place, plate tectonics became generally accepted, and the generation of magmas could now be related to the geodynamic features like convection cells and subduction zones. The other new feature was the development of new analytical apparatus which allowed high accuracy analyses of trace elements and isotopes. In addition it became possible to do ex perimental studies at pressures up to 100 kbar. During the 1970's a large amount of analytical data was obtained and it became evident that the igneous processes that control the compositions of magmas are not that simple to determine. The composition of a magma is controlled by the compositions of its source, the degree of partial melting, and the degree of fractionation. In order to understand the significance of these various processes the relationship between the physical processes and their geochemical consequences should be known. Presently there are several theories that attempt to explain the origin of the various magma types, and these theories can only be evaluated by turning the different ideas into quantitative models. We will so to speak have to do some book keeping for the various theories in order to see which ones are valid. the present book is intended as an introduction to the more fun damental aspects of quantitative igneous petrology. 392 pp. Englisch.
Librería: Majestic Books, Hounslow, Reino Unido
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Añadir al carritoCondición: New. Print on Demand pp. 392 291 Figures, 67:B&W 6.69 x 9.61 in or 244 x 170 mm (Pinched Crown) Perfect Bound on White w/Gloss Lam.
Librería: Biblios, Frankfurt am main, HESSE, Alemania
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Añadir al carritoCondición: New. PRINT ON DEMAND pp. 392.
Idioma: Inglés
Publicado por Springer, Springer Apr 2012, 2012
ISBN 10: 3642493564 ISBN 13: 9783642493560
Librería: buchversandmimpf2000, Emtmannsberg, BAYE, Alemania
EUR 53,49
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Añadir al carritoTaschenbuch. Condición: Neu. This item is printed on demand - Print on Demand Titel. Neuware -Igneous petrology was to some extent essentially a descriptive sci ence until about 1960. The results were mainly obtained from field work, major element analyses, and microscopical studies. During the 1960's two simultaneous developments took place, plate tectonics became generally accepted, and the generation of magmas could now be related to the geodynamic features like convection cells and subduction zones. The other new feature was the development of new analytical apparatus which allowed high accuracy analyses of trace elements and isotopes. In addition it became possible to do ex perimental studies at pressures up to 100 kbar. During the 1970's a large amount of analytical data was obtained and it became evident that the igneous processes that control the compositions of magmas are not that simple to determine. The composition of a magma is controlled by the compositions of its source, the degree of partial melting, and the degree of fractionation. In order to understand the significance of these various processes the relationship between the physical processes and their geochemical consequences should be known. Presently there are several theories that attempt to explain the origin of the various magma types, and these theories can only be evaluated by turning the different ideas into quantitative models. We will so to speak have to do some book keeping for the various theories in order to see which ones are valid. the present book is intended as an introduction to the more fun damental aspects of quantitative igneous petrology.Springer-Verlag KG, Sachsenplatz 4-6, 1201 Wien 392 pp. Englisch.