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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| Những tác giả chính: | , |
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| Định dạng: | Sách |
| Ngôn ngữ: | English |
| Được phát hành: |
Cambridge University Press
2013
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| Những chủ đề: | |
| Truy cập trực tuyến: | http://scholar.dlu.edu.vn/thuvienso/handle/DLU123456789/35562 |
| Các nhãn: |
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| Thư viện lưu trữ: | Thư viện Trường Đại học Đà Lạt |
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| Tóm tắt: | 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). |
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