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Titlebook: Geology and Water; An introduction to f Richard E. Chapman Book 1981 Martinus Nijhoff / Dr. W. Junk Publishers bv, The Hague 1981 Deformati

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发表于 2025-3-21 18:10:32 | 显示全部楼层 |阅读模式
书目名称Geology and Water
副标题An introduction to f
编辑Richard E. Chapman
视频video
丛书名称Developments in Applied Earth Studies
图书封面Titlebook: Geology and Water; An introduction to f Richard E. Chapman Book 1981 Martinus Nijhoff / Dr. W. Junk Publishers bv, The Hague 1981 Deformati
描述Water is one of the world‘s threatened resources: it is also a substance of importance in Geology. For some years I have felt the need for a book that sets out the fundamentals of fluid mechanics, written for geologists rather than engineers. The efforts to repair my own deficiencies in this respect led me along various unfamiliar paths, few of which were unrewarding. This book is the result of my journeys through the literature and as a geologist in several parts of the world. It has been written for students of geology of all ages, in the simplest terms possible, and it has one objective: to provide a basis for an understanding of the mechanical role of water in geology. It has not been written for experts in ground­ water hydrology, or specialists in the fluid aspects of structural geology: it has been written for geologists like me who are not very good mathematicians, so that we can take water better into account in our normal geological work, whatever it might be. The fundamentals apply equally to mineralization, geochemistry, and vulcanology although they have not been specifically mentioned. It has also been written for the university student of geology so that he or she ma
出版日期Book 1981
关键词Deformation; Drainage; Fundament; fluid mechanics; geochemistry; geology; hydrology; mineral; rivers; sedimen
版次1
doihttps://doi.org/10.1007/978-94-009-8244-4
isbn_softcover978-94-009-8246-8
isbn_ebook978-94-009-8244-4
copyrightMartinus Nijhoff / Dr. W. Junk Publishers bv, The Hague 1981
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Pore Water and Sliding,res. On the other hand, if the block slides down a slope under the force of gravity, the previous difficulty is replaced by two others: the coefficient of friction of rock on rock suggests that an angle of about 30° would be required for gravitational sliding — and that also implies a vertical relie
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Role of Pore Water in Deformation of Sedimentary Basins, that important deformation occurs in sedimentary basins while they are accumulating sediment on a subsiding sedimentary column — particularly in the terminal regressive sequence. The regressive sequence itself is due to a neighbouring orogeny outside the sedimentary basin: the creation of mountains
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