Rock Stress and Its Measurement

O. Stephansson

ISBN 10: 0412447002 / ISBN 13: 9780412447006

Published by Springer Netherlands Mrz 1997, 1997

About this Item

This item is printed on demand - it takes 3-4 days longer - Neuware -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. 512 pp. Englisch.

Seller Inventory # 9780412447006

Bibliographic Details

• Title: Rock Stress and Its Measurement
• Publisher: Springer Netherlands Mrz 1997
• Publication Date: 1997
• Language: English
• ISBN 10: 0412447002
• ISBN 13: 9780412447006
• Binding: Buch
• Condition: Neu
• Dimensions: 260W x 183H x 33D millimeters 260 millimeters width by 183 millimeters height by 33 millimeters depth
• Weight: 1150 grams

About this title

Synopsis

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.

Review

`...of great interest...'
Australian Mineral Foundation Reviews