Glacially-triggered faulting:
Glacially triggered faulting describes movement of pre-existing faults caused by a combination of tectonic and glacially induced isostatic stresses. The most impressive fault-scarps are found in northern Europe, assumed to be reactivated at the end of the deglaciation. This view has been challenged...
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| Weitere beteiligte Personen: | , , |
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| Format: | E-Book |
| Sprache: | Englisch |
| Veröffentlicht: |
Cambridge
Cambridge University Press
2022
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| Links: | https://doi.org/10.1017/9781108779906 |
| Zusammenfassung: | Glacially triggered faulting describes movement of pre-existing faults caused by a combination of tectonic and glacially induced isostatic stresses. The most impressive fault-scarps are found in northern Europe, assumed to be reactivated at the end of the deglaciation. This view has been challenged as new faults have been discovered globally with advanced techniques such as LiDAR, and fault activity dating has shown several phases of reactivation thousands of years after deglaciation ended. This book summarizes the current state-of-the-art research in glacially triggered faulting, discussing the theoretical aspects that explain the presence of glacially induced structures and reviews the geological, geophysical, geodetic and geomorphological investigation methods. Written by a team of international experts, it provides the first global overview of confirmed and proposed glacially induced faults, and provides an outline for modelling these stresses and features. It is a go-to reference for geoscientists and engineers interested in ice sheet-solid Earth interaction. |
| Umfang: | 1 Online-Ressource (xxii, 438 Seiten) |
| ISBN: | 9781108779906 |
Internformat
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| 520 | |a Glacially triggered faulting describes movement of pre-existing faults caused by a combination of tectonic and glacially induced isostatic stresses. The most impressive fault-scarps are found in northern Europe, assumed to be reactivated at the end of the deglaciation. This view has been challenged as new faults have been discovered globally with advanced techniques such as LiDAR, and fault activity dating has shown several phases of reactivation thousands of years after deglaciation ended. This book summarizes the current state-of-the-art research in glacially triggered faulting, discussing the theoretical aspects that explain the presence of glacially induced structures and reviews the geological, geophysical, geodetic and geomorphological investigation methods. Written by a team of international experts, it provides the first global overview of confirmed and proposed glacially induced faults, and provides an outline for modelling these stresses and features. It is a go-to reference for geoscientists and engineers interested in ice sheet-solid Earth interaction. | ||
| 700 | 1 | |a Olesen, Odleiv | |
| 700 | 1 | |a Steffen, Holger | |
| 700 | 1 | |a Sutinen, Raimo | |
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Datensatz im Suchindex
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| id | ZDB-20-CTM-CR9781108779906 |
| illustrated | Not Illustrated |
| indexdate | 2025-03-19T15:54:06Z |
| institution | BVB |
| isbn | 9781108779906 |
| language | English |
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| physical | 1 Online-Ressource (xxii, 438 Seiten) |
| psigel | ZDB-20-CTM TUM_PDA_CTM ZDB-20-CTM |
| publishDate | 2022 |
| publishDateSearch | 2022 |
| publishDateSort | 2022 |
| publisher | Cambridge University Press |
| record_format | marc |
| spelling | Glacially-triggered faulting edited by Holger Steffen, Odleiv Olesen, Raimo Sutinen Cambridge Cambridge University Press 2022 1 Online-Ressource (xxii, 438 Seiten) txt c cr Glacially triggered faulting describes movement of pre-existing faults caused by a combination of tectonic and glacially induced isostatic stresses. The most impressive fault-scarps are found in northern Europe, assumed to be reactivated at the end of the deglaciation. This view has been challenged as new faults have been discovered globally with advanced techniques such as LiDAR, and fault activity dating has shown several phases of reactivation thousands of years after deglaciation ended. This book summarizes the current state-of-the-art research in glacially triggered faulting, discussing the theoretical aspects that explain the presence of glacially induced structures and reviews the geological, geophysical, geodetic and geomorphological investigation methods. Written by a team of international experts, it provides the first global overview of confirmed and proposed glacially induced faults, and provides an outline for modelling these stresses and features. It is a go-to reference for geoscientists and engineers interested in ice sheet-solid Earth interaction. Olesen, Odleiv Steffen, Holger Sutinen, Raimo Erscheint auch als Druck-Ausgabe 9781108490023 |
| spellingShingle | Glacially-triggered faulting |
| title | Glacially-triggered faulting |
| title_auth | Glacially-triggered faulting |
| title_exact_search | Glacially-triggered faulting |
| title_full | Glacially-triggered faulting edited by Holger Steffen, Odleiv Olesen, Raimo Sutinen |
| title_fullStr | Glacially-triggered faulting edited by Holger Steffen, Odleiv Olesen, Raimo Sutinen |
| title_full_unstemmed | Glacially-triggered faulting edited by Holger Steffen, Odleiv Olesen, Raimo Sutinen |
| title_short | Glacially-triggered faulting |
| title_sort | glacially triggered faulting |
| work_keys_str_mv | AT olesenodleiv glaciallytriggeredfaulting AT steffenholger glaciallytriggeredfaulting AT sutinenraimo glaciallytriggeredfaulting |