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Titlebook: Geodynamics of the Lithosphere; An Introduction Kurt Stüwe Textbook 2007Latest edition Springer-Verlag Berlin Heidelberg 2007 Deformation.G

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書目名稱Geodynamics of the Lithosphere
副標題An Introduction
編輯Kurt Stüwe
視頻videohttp://file.papertrans.cn/384/383129/383129.mp4
概述Clear representation of the subject for the field oriented geologist.Artwork specially designed for this book.Qualitative representation of geodynamical processes
圖書封面Titlebook: Geodynamics of the Lithosphere; An Introduction Kurt Stüwe Textbook 2007Latest edition Springer-Verlag Berlin Heidelberg 2007 Deformation.G
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 quite loosely, the methods of their description involve well defined fields. Energetic descriptions are involved with distribu- tion of energy in our planet, typically expressed in terms of heat and tempera- ture. Kinematic descriptions describe movements using velocities, strains and strain rates. Dynamic descriptions indicate how stresses and forces behave. In the field, we document only the consequences of geological processes. The underlying causes are much harder to constrain directly. Nevertheless, if we want to explain the tectonic evolution of our planet, we need to interpret these causes or: "driving forces" . For this, we need to find a dynamic description of geological processes that is consistent with our observations. 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 observations in nature. As we wil
出版日期Textbook 2007Latest edition
關(guān)鍵詞Deformation; Geoinformationssysteme; Lithosphere; Lithosph?re; Rheologie; Rheology; geomorphology; mechanic
版次2
doihttps://doi.org/10.1007/978-3-540-71237-4
isbn_softcover978-3-642-44814-0
isbn_ebook978-3-540-71237-4
copyrightSpringer-Verlag Berlin Heidelberg 2007
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Introduction,istribution of energy in our planet, typically expressed in terms of heat and temperature. . descriptions describe movements using velocities, strains and strain rates. . descriptions indicate how stresses and forces behave.
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Plate Tectonics, presented. 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 remainder of the book. As such, the chapter is meant as a basis for all following chapters.
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geodynamical processesThe 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 quite loosely, the methods
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978-3-642-44814-0Springer-Verlag Berlin Heidelberg 2007
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https://doi.org/10.1007/978-3-540-71237-4Deformation; Geoinformationssysteme; Lithosphere; Lithosph?re; Rheologie; Rheology; geomorphology; mechanic
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