Overview
- Authors:
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Bernard Amadei
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Department of Civil, Environmental and Architectural Engineering, University of Colorado, Boulder, USA
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Ove Stephansson
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Department of Civil and Environmental Engineering, Royal Institute of Technology, Stockholm, Sweden
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Table of contents (12 chapters)
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- Bernard Amadei, Ove Stephansson
Pages 1-21
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- Bernard Amadei, Ove Stephansson
Pages 23-94
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- Bernard Amadei, Ove Stephansson
Pages 95-120
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- Bernard Amadei, Ove Stephansson
Pages 121-199
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- Bernard Amadei, Ove Stephansson
Pages 201-276
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- Bernard Amadei, Ove Stephansson
Pages 277-288
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- Bernard Amadei, Ove Stephansson
Pages 289-302
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- Bernard Amadei, Ove Stephansson
Pages 303-325
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- Bernard Amadei, Ove Stephansson
Pages 327-360
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- Bernard Amadei, Ove Stephansson
Pages 361-385
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- Bernard Amadei, Ove Stephansson
Pages 387-417
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- Bernard Amadei, Ove Stephansson
Pages 419-460
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Back Matter
Pages 461-490
About this book
Rock masses are initially stressed in their current in situ state of stress and to a lesser natural state. Whether one is interested in the extent on the monitoring of stress change. formation of geological structures (folds, faults, The subject of paleostresses is only briefly intrusions, etc. ), the stability of artificial struc discussed. tures (tunnels, caverns, mines, surface excava The last 30 years have seen a major advance our knowledge and understanding of rock tions, etc. ), or the stability of boreholes, a in the in situ or virgin stress field, stress. A large body of data is now available on knowledge of along with other rock mass properties, is the state of stress in the near surface of the needed in order to predict the response of rock Earth's crust (upper 3-4km of the crust). masses to the disturbance associated with those Various theories have been proposed regarding structures. Stress in rock is usually described the origin of in situ stresses and how gravity, within the context of continuum mechanics. It is tectonics, erosion, lateral straining, rock fabric, defined at a point and is represented by a glaciation and deglaciation, topography, curva second-order Cartesian tensor with six compo ture of the Earth and other active geological nents. Because of its definition, rock stress is an features and processes contribute to the current enigmatic and fictitious quantity creating chal in situ stress field.
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`...of great interest...'
Australian Mineral Foundation Reviews
Authors and Affiliations
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Department of Civil, Environmental and Architectural Engineering, University of Colorado, Boulder, USA
Bernard Amadei
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Department of Civil and Environmental Engineering, Royal Institute of Technology, Stockholm, Sweden
Ove Stephansson