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Titlebook: Geodynamics of the Lithosphere; Kurt Stüwe Textbook 20021st edition Springer-Verlag Berlin Heidelberg 2002 Approximation.Deformation.Litho

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发表于 2025-3-21 18:57:06 | 显示全部楼层 |阅读模式
书目名称Geodynamics of the Lithosphere
编辑Kurt Stüwe
视频video
概述Clear representation of the subject for the field oriented geologist.Artwork specially designed for this book.Qualitative representation of geodynamical processes
图书封面Titlebook: Geodynamics of the Lithosphere;  Kurt Stüwe Textbook 20021st edition Springer-Verlag Berlin Heidelberg 2002 Approximation.Deformation.Litho
描述The large scale structure of the earth is caused by geodynamic processes which are explained using energetic, kinematic and dynamic descriptions. While "geodynamic processes" are understood to include a large variety of processes and the term is used by earth scientists quite loosely, the methods of their description involve well defined fields. Energetic descriptions are in­ volved with distribution of energy in our planet, typically expressed in terms of heat and temperature. Kinematic descriptions describe movements using velocities, strains and strain rates and Dynamic descriptions indicate how stresses and forces behave. As structural and metamorphic geologists we document in the field only the consequences of geological processes. The underlying causes are much harder to constrain directly. However, it is absolutely crucial to understand these causes or: "driving forces", if we are to explain the tectonic evolution of our planet. This book deals with the dynamic description of geological processes. Our descriptions relate causes and consequences - tectonic processes with field observations. In many cases, we will use equations as a concise form to describe processes and obser
出版日期Textbook 20021st edition
关键词Approximation; Deformation; Lithosphere; Lithosphäre; Rheologie; Rheology; geomorphology; mechanical modell
版次1
doihttps://doi.org/10.1007/978-3-662-04980-8
isbn_ebook978-3-662-04980-8
copyrightSpringer-Verlag Berlin Heidelberg 2002
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发表于 2025-3-21 20:32:54 | 显示全部楼层
Die Methode der finiten Elemente of any present day mountain range on this planet that is this high and that, therefore, this interpretation is unlikely. However, in many less obvious examples there are no direct analogies and the resulting models — albeit perfectly imaginable and fully consistent with field observations — are wro
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ing forces", if we are to explain the tectonic evolution of our planet. This book deals with the dynamic description of geological processes. Our descriptions relate causes and consequences - tectonic processes with field observations. In many cases, we will use equations as a concise form to describe processes and obser978-3-662-04980-8
发表于 2025-3-22 04:43:02 | 显示全部楼层
Force and Rheology, of any present day mountain range on this planet that is this high and that, therefore, this interpretation is unlikely. However, in many less obvious examples there are no direct analogies and the resulting models — albeit perfectly imaginable and fully consistent with field observations — are wro
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Erratum to: Beispiele aus der Praxis,nclude a large variety of . and the term is used by earth scientists quite loosely, the methods of their . involve well defined fields. . descriptions are involved with distribution of energy in our planet, typically expressed in terms of heat and temperature. . descriptions describe movements using
发表于 2025-3-22 20:10:18 | 显示全部楼层
https://doi.org/10.1007/978-3-662-28961-7 exiting conceptual model and discuss some basic principles how to describe it. In the second part of this chapter we discuss the layered structure of the earth and the geographic distribution of lithospheric plates. We will also use this chapter to introduce the terminology that is used in the rema
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Die Ziele der Forstwirthschaft, elevation of mountain ranges, and the depth of the oceans, as well as the . of such parameters: kinematics. We begin with a consideration of different coordinate systems and reference frames that we will use.
发表于 2025-3-23 07:04:50 | 显示全部楼层
Die Methode der finiten Elementerogens, provide a useful independent constraint on models based on field observations. Let us consider an example: A field geologist finds in a Precambrian shield folds and thrusts that he interprets to have formed as the consequence of crustal shortening. A detailed strain analysis shows that 80% s
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