| 書目名稱 | Rock Stress and Its Measurement | | 編輯 | Bernard Amadei,Ove Stephansson | | 視頻video | http://file.papertrans.cn/832/831436/831436.mp4 | | 圖書封面 |  | | 描述 | 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 | | 出版日期 | Book 1997 | | 關(guān)鍵詞 | Borehole; concrete; geology; geophysics; mining; structural geology; economic geology | | 版次 | 1 | | doi | https://doi.org/10.1007/978-94-011-5346-1 | | isbn_softcover | 978-94-010-6247-3 | | isbn_ebook | 978-94-011-5346-1 | | copyright | Springer Science+Business Media Dordrecht 1997 |
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