Modern Methods Geochemical Analysis (11 results)

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    • Language: English

      Published by Springer, 2012

      1468418327 / 9781468418323

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      Seller: Ria Christie Collections, Uxbridge, United KingdomRia Christie Collections

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    • Language: English

      Published by Springer US, 2012

      1468418327 / 9781468418323

      • Softcover

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    • Language: English

      Published by Springer, 2012

      1468418327 / 9781468418323

      • Softcover

      Seller: Books Puddle, New York, NY, U.S.A.Books Puddle

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      Condition: New. pp. 416.

    • Language: English

      Published by Springer, 2013

      1468418327 / 9781468418323

      • Softcover

      Seller: Revaluation Books, Exeter, United KingdomRevaluation Books

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      Paperback. Condition: Brand New. reprint edition. 416 pages. 9.02x5.98x0.94 inches. In Stock.

    • Language: English

      Published by Springer, Springer New York, 2012

      1468418327 / 9781468418323

      • Softcover

      Seller: AHA-BUCH GmbH, Einbeck, GermanyAHA-BUCH GmbH

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      Taschenbuch. Condition: Neu. Druck auf Anfrage Neuware - Printed after ordering - The founders of geology at the beginning of the last century were suspicious oflaboratories. Hutton's well-known dictum illustrates the point: 'There are also superficial reasoning men . . . they judge of the great oper ations of the mineral kingdom from having kindled a fire, and looked into the bottom of a little crucible. ' The idea was not unreasonable; the earth is so large and its changes are so slow and so complicated that labo ratory tests and experiments were of little help. The earth had to be studied in its own terms and geology grew up as a separate science and not as a branch of physics or chemistry. Its practitioners were, for the most part, experts in structure, stratigraphy, or paleontology, not in silicate chemistry or mechanics. The chemists broke into this closed circle before the physicists did. The problems of the classification of rocks, particularly igneous rocks, and of the nature and genesis of ores are obviously chemical and, by the mid- 19th century, chemistry was in a state where rocks could be effectively analyzed, and a classification built up depending partly on chemistry and partly on the optical study of thin specimens. Gradually the chemical study of rocks became one of the central themes of earth science.

    • Language: English

      Published by Springer, 2012

      1468418327 / 9781468418323

      • Softcover

      Seller: Mispah books, Redhill, SURRE, United KingdomMispah books

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    • Language: English

      Published by Springer, 2012

      1468418327 / 9781468418323

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      Seller: Brook Bookstore On Demand, Napoli, NA, ItalyBrook Bookstore On Demand

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    • Language: English

      Published by Springer, Springer Dez 2012, 2012

      1468418327 / 9781468418323

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      Seller: BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, GermanyBuchWeltWeit Ludwig Meier e.K.

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      Taschenbuch. Condition: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -The founders of geology at the beginning of the last century were suspicious oflaboratories. Hutton's well-known dictum illustrates the point: 'There are also superficial reasoning men . . . they judge of the great oper ations of the mineral kingdom from having kindled a fire, and looked into the bottom of a little crucible. ' The idea was not unreasonable; the earth is so large and its changes are so slow and so complicated that labo ratory tests and experiments were of little help. The earth had to be studied in its own terms and geology grew up as a separate science and not as a branch of physics or chemistry. Its practitioners were, for the most part, experts in structure, stratigraphy, or paleontology, not in silicate chemistry or mechanics. The chemists broke into this closed circle before the physicists did. The problems of the classification of rocks, particularly igneous rocks, and of the nature and genesis of ores are obviously chemical and, by the mid- 19th century, chemistry was in a state where rocks could be effectively analyzed, and a classification built up depending partly on chemistry and partly on the optical study of thin specimens. Gradually the chemical study of rocks became one of the central themes of earth science. 416 pp. Englisch.

    • Language: English

      Published by Springer, 2012

      1468418327 / 9781468418323

      • Softcover
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      Seller: Majestic Books, Hounslow, United KingdomMajestic Books

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      Condition: New. Print on Demand pp. 416 23:B&W 6 x 9 in or 229 x 152 mm Perfect Bound on White w/Gloss Lam.

    • Language: English

      Published by Springer, 2012

      1468418327 / 9781468418323

      • Softcover
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      Seller: Biblios, frankfurt am main, HESSE, GermanyBiblios

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      Condition: New. PRINT ON DEMAND pp. 416.

    • Language: English

      Published by Springer, Springer New York Dez 2012, 2012

      1468418327 / 9781468418323

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      Seller: buchversandmimpf2000, Emtmannsberg, BAYE, Germanybuchversandmimpf2000

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      Taschenbuch. Condition: Neu. This item is printed on demand - Print on Demand Titel. Neuware -The founders of geology at the beginning of the last century were suspicious oflaboratories. Hutton's well-known dictum illustrates the point: 'There are also superficial reasoning men . . . they judge of the great oper ations of the mineral kingdom from having kindled a fire, and looked into the bottom of a little crucible. ' The idea was not unreasonable; the earth is so large and its changes are so slow and so complicated that labo ratory tests and experiments were of little help. The earth had to be studied in its own terms and geology grew up as a separate science and not as a branch of physics or chemistry. Its practitioners were, for the most part, experts in structure, stratigraphy, or paleontology, not in silicate chemistry or mechanics. The chemists broke into this closed circle before the physicists did. The problems of the classification of rocks, particularly igneous rocks, and of the nature and genesis of ores are obviously chemical and, by the mid- 19th century, chemistry was in a state where rocks could be effectively analyzed, and a classification built up depending partly on chemistry and partly on the optical study of thin specimens. Gradually the chemical study of rocks became one of the central themes of earth science.Springer-Verlag KG, Sachsenplatz 4-6, 1201 Wien 416 pp. Englisch.