Geophysical Continua Deformation in the Earth’s Interior
The development of quantitative methods for the study of the Earth rests firmly on the application of physical techniques to the properties of materials without recourse to the details of atomic level structure. This has formed the basis of seismological methods for investigating the internal str...
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Cambridge University Press
2013
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| Truy cập trực tuyến: | http://scholar.dlu.edu.vn/thuvienso/handle/DLU123456789/35562 |
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oai:scholar.dlu.edu.vn:DLU123456789-355622014-01-19T23:46:19Z Geophysical Continua Deformation in the Earth’s Interior Kennett, B. L. N Bunge, H.-P Geophysical Deformation The development of quantitative methods for the study of the Earth rests firmly on the application of physical techniques to the properties of materials without recourse to the details of atomic level structure. This has formed the basis of seismological methods for investigating the internal structure of the Earth, and for modelling of mantle convection through fluid flow. The deformation behaviour of materials is inextricably tied to microscopic properties such as the elasticity of individual crystals and processes such as the movement of dislocations. In the continuum representation such microscopic behaviour is encapsulated in the description of the rheology of the material through the connection between stress and strain (or strain rate). 2013-09-16T08:53:50Z 2013-09-16T08:53:50Z 2008 Book 978-0-511-40890-8 http://scholar.dlu.edu.vn/thuvienso/handle/DLU123456789/35562 en application/pdf Cambridge University Press |
| institution |
Thư viện Trường Đại học Đà Lạt |
| collection |
Thư viện số |
| language |
English |
| topic |
Geophysical Deformation |
| spellingShingle |
Geophysical Deformation Kennett, B. L. N Bunge, H.-P Geophysical Continua Deformation in the Earth’s Interior |
| description |
The development of quantitative methods for the study of the Earth rests firmly
on the application of physical techniques to the properties of materials without
recourse to the details of atomic level structure. This has formed the basis of
seismological methods for investigating the internal structure of the Earth, and for
modelling of mantle convection through fluid flow. The deformation behaviour
of materials is inextricably tied to microscopic properties such as the elasticity
of individual crystals and processes such as the movement of dislocations. In
the continuum representation such microscopic behaviour is encapsulated in the
description of the rheology of the material through the connection between stress
and strain (or strain rate). |
| format |
Book |
| author |
Kennett, B. L. N Bunge, H.-P |
| author_facet |
Kennett, B. L. N Bunge, H.-P |
| author_sort |
Kennett, B. L. N |
| title |
Geophysical Continua
Deformation in the Earth’s Interior |
| title_short |
Geophysical Continua
Deformation in the Earth’s Interior |
| title_full |
Geophysical Continua
Deformation in the Earth’s Interior |
| title_fullStr |
Geophysical Continua
Deformation in the Earth’s Interior |
| title_full_unstemmed |
Geophysical Continua
Deformation in the Earth’s Interior |
| title_sort |
geophysical continua
deformation in the earth’s interior |
| publisher |
Cambridge University Press |
| publishDate |
2013 |
| url |
http://scholar.dlu.edu.vn/thuvienso/handle/DLU123456789/35562 |
| _version_ |
1757675541094203392 |