Rock Stress and Its Measurement:
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. ), t...
Gespeichert in:
| Hauptverfasser: | , |
|---|---|
| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Dordrecht
Springer Netherlands
1997
|
| Schlagworte: | |
| Online-Zugang: | BTU01 URL des Erstveröffentlichers |
| Zusammenfassung: | 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 |
| Beschreibung: | 1 Online-Ressource (XV, 490 p) |
| ISBN: | 9789401153461 |
| DOI: | 10.1007/978-94-011-5346-1 |
Internformat
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| 520 | |a 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 | ||
| 650 | 4 | |a Engineering | |
| 650 | 4 | |a Geoengineering, Foundations, Hydraulics | |
| 650 | 4 | |a Geomorphology | |
| 650 | 4 | |a Geotechnical Engineering & Applied Earth Sciences | |
| 650 | 4 | |a Structural Geology | |
| 650 | 4 | |a Economic Geology | |
| 650 | 4 | |a Engineering | |
| 650 | 4 | |a Economic geology | |
| 650 | 4 | |a Structural geology | |
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Datensatz im Suchindex
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| author | Amadei, Bernard Stephansson, Ove |
| author_facet | Amadei, Bernard Stephansson, Ove |
| author_role | aut aut |
| author_sort | Amadei, Bernard |
| author_variant | b a ba o s os |
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| bvnumber | BV045185023 |
| collection | ZDB-2-ENG |
| ctrlnum | (ZDB-2-ENG)978-94-011-5346-1 (OCoLC)1184444639 (DE-599)BVBBV045185023 |
| dewey-full | 624.15 |
| dewey-hundreds | 600 - Technology (Applied sciences) |
| dewey-ones | 624 - Civil engineering |
| dewey-raw | 624.15 |
| dewey-search | 624.15 |
| dewey-sort | 3624.15 |
| dewey-tens | 620 - Engineering and allied operations |
| discipline | Bauingenieurwesen |
| doi_str_mv | 10.1007/978-94-011-5346-1 |
| format | Electronic eBook |
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| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:54Z |
| institution | BVB |
| isbn | 9789401153461 |
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| publishDate | 1997 |
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| spelling | Amadei, Bernard Verfasser aut Rock Stress and Its Measurement by Bernard Amadei, Ove Stephansson Dordrecht Springer Netherlands 1997 1 Online-Ressource (XV, 490 p) txt rdacontent c rdamedia cr rdacarrier 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 Engineering Geoengineering, Foundations, Hydraulics Geomorphology Geotechnical Engineering & Applied Earth Sciences Structural Geology Economic Geology Economic geology Structural geology Geotechnical engineering Engineering geology Engineering / Geology Foundations Hydraulics Spannung Geologie (DE-588)4381340-9 gnd rswk-swf Messung (DE-588)4038852-9 gnd rswk-swf Spannung Geologie (DE-588)4381340-9 s Messung (DE-588)4038852-9 s 1\p DE-604 Stephansson, Ove aut Erscheint auch als Druck-Ausgabe 9789401062473 https://doi.org/10.1007/978-94-011-5346-1 Verlag URL des Erstveröffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
| spellingShingle | Amadei, Bernard Stephansson, Ove Rock Stress and Its Measurement Engineering Geoengineering, Foundations, Hydraulics Geomorphology Geotechnical Engineering & Applied Earth Sciences Structural Geology Economic Geology Economic geology Structural geology Geotechnical engineering Engineering geology Engineering / Geology Foundations Hydraulics Spannung Geologie (DE-588)4381340-9 gnd Messung (DE-588)4038852-9 gnd |
| subject_GND | (DE-588)4381340-9 (DE-588)4038852-9 |
| title | Rock Stress and Its Measurement |
| title_auth | Rock Stress and Its Measurement |
| title_exact_search | Rock Stress and Its Measurement |
| title_full | Rock Stress and Its Measurement by Bernard Amadei, Ove Stephansson |
| title_fullStr | Rock Stress and Its Measurement by Bernard Amadei, Ove Stephansson |
| title_full_unstemmed | Rock Stress and Its Measurement by Bernard Amadei, Ove Stephansson |
| title_short | Rock Stress and Its Measurement |
| title_sort | rock stress and its measurement |
| topic | Engineering Geoengineering, Foundations, Hydraulics Geomorphology Geotechnical Engineering & Applied Earth Sciences Structural Geology Economic Geology Economic geology Structural geology Geotechnical engineering Engineering geology Engineering / Geology Foundations Hydraulics Spannung Geologie (DE-588)4381340-9 gnd Messung (DE-588)4038852-9 gnd |
| topic_facet | Engineering Geoengineering, Foundations, Hydraulics Geomorphology Geotechnical Engineering & Applied Earth Sciences Structural Geology Economic Geology Economic geology Structural geology Geotechnical engineering Engineering geology Engineering / Geology Foundations Hydraulics Spannung Geologie Messung |
| url | https://doi.org/10.1007/978-94-011-5346-1 |
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