Titlebook: Rock Stress and Its Measurement; Bernard Amadei,Ove Stephansson Book 1997 Springer Science+Business Media Dordrecht 1997 Borehole.concrete

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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

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Estimating , Stresses, or geological structures (faults, folds, shear zones, uncomformities, volcanic vents and dikes). Estimating . stresses can be useful in the early stage of engineering design, for the planning process and when selecting stress measuring methods and the location of those measurements.

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Strain Recovery Methods,ins (Fig. 7.1a). Determination of the magnitude of the stresses is more difficult and requires a constitutive model for the rock. This relatively recent stress measurement method is called the ‘anelastic strain recovery’ (ASR) method.

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Book 2011Latest edition städtischen Arealen. Welchen Einfluss üben die verschiedenen großstädtischen Quartiere hierbei aus? Gibt es Zusammenhänge zwischen Architektur und Städtischer Entwicklung und Planung und dem Gewaltphänomen im Jugendalter?.Mit Hilfe eines typologischen Konzeptes werden die Zusammenhänge von städtisc