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Titlebook: Modern Methods of Geochemical Analysis; Richard E. Wainerdi (Associate Dean of Engineering Book 1971 Springer Science+Business Media New Y

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发表于 2025-3-21 19:35:00 | 显示全部楼层 |阅读模式
书目名称Modern Methods of Geochemical Analysis
编辑Richard E. Wainerdi (Associate Dean of Engineering
视频video
丛书名称Monographs in Geoscience
图书封面Titlebook: Modern Methods of Geochemical Analysis;  Richard E. Wainerdi (Associate Dean of Engineering Book 1971 Springer Science+Business Media New Y
描述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 stud
出版日期Book 1971
关键词Stratigraphy; chemical analysis; chemistry; classification; geochemistry; geology; geoscience; igneous rock
版次1
doihttps://doi.org/10.1007/978-1-4684-1830-9
isbn_softcover978-1-4684-1832-3
isbn_ebook978-1-4684-1830-9
copyrightSpringer Science+Business Media New York 1971
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发表于 2025-3-21 23:43:20 | 显示全部楼层
eous 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 stud978-1-4684-1832-3978-1-4684-1830-9
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978-1-4684-1832-3Springer Science+Business Media New York 1971
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Book 1971are 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 te
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t: "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
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https://doi.org/10.1007/978-3-662-05645-5Algebra; Galois-Theorie; Galoistheorie; Gruppentheorie; Konstruktion mit Zirkel und Lineal; Körpertheorie
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