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Titlebook: Atlas of Photomicrographs of the Surface Structures of Lunar Regolith Particles; O. D. Rode,A. V. Ivanov,В. Гейл Book 1979 Springer Scienc

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發(fā)表于 2025-3-21 18:00:12 | 只看該作者 |倒序瀏覽 |閱讀模式
期刊全稱Atlas of Photomicrographs of the Surface Structures of Lunar Regolith Particles
影響因子2023O. D. Rode,A. V. Ivanov,В. Гейл
視頻videohttp://file.papertrans.cn/165/164431/164431.mp4
圖書封面Titlebook: Atlas of Photomicrographs of the Surface Structures of Lunar Regolith Particles;  O. D. Rode,A. V. Ivanov,В. Гейл Book 1979 Springer Scienc
影響因子The rapid evolution of technology and mathematical methods in this century has led to the recognition and accumulation of a large quantity of scientific facts. At the same time, however, in studying natural bodies, primary attention has not been paid to their total character; the body either ceased to be an individual, as in the case of mathematical methods, or has become a complex of separate, not always closely connected characteristics examined by laboratory analyses. The goniometric study of a crystal, for example, has developed into the determination of constants of the crystal lattice, but the examination of minerals from a specific deposit was concerned primarily with the chemical analysis of their admixtures. In geological sciences a thorough morphological investigation has preserved its original importance, particularly in geomorphology and paleontology. Even in petrography, the three-dimensional description of rocks was replaced by the study of thin sections, since the optical microscope does not permit examination of an uneven surface as a result of a restricted depth of observation field. The art of ancient naturalists of conceiving the object in its entirety, with all
Pindex Book 1979
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Atlas of Photomicrographs of the Surface Structures of Lunar Regolith Particles978-94-009-9359-4
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Book 1979 three-dimensional description of rocks was replaced by the study of thin sections, since the optical microscope does not permit examination of an uneven surface as a result of a restricted depth of observation field. The art of ancient naturalists of conceiving the object in its entirety, with all
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https://doi.org/10.1007/1-84628-252-7h was transported from the place of its original occurrence. This heterogeneous mixture, dark-gray or black in the maria and light-gray in the highlands, consists of minute fragments of crystalline rocks and minerals, of welded and brecciated agglomerates and partly melted particles. The average siz
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https://doi.org/10.1007/978-94-009-9359-4evolution; geomorphology; mineral; petrography
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