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Titlebook: Introduction to Mineralogy; Crystallography and Carl W. Correns Textbook 19691st edition Springer-Verlag Berlin Heidelberg 1969 chemistry.

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書(shū)目名稱Introduction to Mineralogy
副標(biāo)題Crystallography and
編輯Carl W. Correns
視頻videohttp://file.papertrans.cn/474/473910/473910.mp4
圖書(shū)封面Titlebook: Introduction to Mineralogy; Crystallography and  Carl W. Correns Textbook 19691st edition Springer-Verlag Berlin Heidelberg 1969 chemistry.
描述The first edition of this book has been out of print for seven years. The ques- tion as to whether a new edition should be produced was answered affirmatively on many counts. I think that the considerations which led me to write this book in 1949 are still valid (see Preface to the First Edition). Moreover, a description of those areas of interest which together comprise the field of Mineralogy seems to be more necessary than ever, because of the rapid advances which have been made. Due to the rapid extension of our knowledge, I did not dare again to treat the whole field by myself. Accordingly, Professor ZEMANN kindly agreed to revise the first part of the book dealing with Crystallography. He made many important corrections. In Part II the basic question arose as to whether the physical-chemical approach to rock forming processes, becoming more and more important, required inclusive treatment of the fundamentals of physical chemistry in the book. I see certain dangers in trying to produce a petrology text which is physical chemically self-sufficient. Thus, I retain the same opinion which prevailed when I wrote the previous edition; namely that the necessary basic knowledge should
出版日期Textbook 19691st edition
關(guān)鍵詞chemistry; crystallography; mineral; mineralogy; petrology
版次1
doihttps://doi.org/10.1007/978-3-642-87134-4
isbn_ebook978-3-642-87134-4
copyrightSpringer-Verlag Berlin Heidelberg 1969
The information of publication is updating

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Crystal Physicss with the field of crystal physics, a borderline area between physics, crystallography, and mineralogy in its most restricted sense. As is true of every interdisciplinary field, the resulting overlap of ideas is desirable and beneficial. The researcher who approaches the subject from pure physics i
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Some Physical-Chemical Fundamentalsn, “When does a crystal crystallize from a melt?”. The obvious answer is that it occurs when a fluid is cooled a bit below the melting temperature (melting point) which prevails at some definite pressure. In order to determine the exact melting point in those cases where it is not possible to direct
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Weathering and Soil Mineral Formationroducts, are quite different from those which produce igneous rocks. Those alteration processes which take place at the surface of the earth, at the earth-atmosphere interface, are called weathering processes. Weathering products formed in situ without transport form soils; following transport they
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Geochemical Considerationsocks in the earth’s crust. Thus, we have observed a cycle of processes starting with magmatic crystallization, leading to weathering, sedimentation, and finally metamorphism, which can lead in turn to the generation of new magmas. In dealing with this so-called rock cycle (or geochemical cycle) we h
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