Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach
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Springer Netherlands
2008
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Online Access: | http://dx.doi.org/10.1007/978-1-4020-6815-7_18 http://link.springer.com/content/pdf/10.1007/978-1-4020-6815-7_18.pdf |
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crspringernat:10.1007/978-1-4020-6815-7_18 2024-03-10T08:35:48+00:00 Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach Kebeasy, T. R. M. Husebye, Eystein S. Hestholm, S. 2008 http://dx.doi.org/10.1007/978-1-4020-6815-7_18 http://link.springer.com/content/pdf/10.1007/978-1-4020-6815-7_18.pdf unknown Springer Netherlands NATO Science Series: IV: Earth and Environmental Sciences Earthquake Monitoring and Seismic Hazard Mitigation in Balkan Countries page 271-289 ISSN 1568-1238 ISBN 9781402068133 9781402068157 book-chapter 2008 crspringernat https://doi.org/10.1007/978-1-4020-6815-7_18 2024-02-13T17:12:42Z Book Part Lurøy Springer Nature Lurøy ENVELOPE(12.849,12.849,66.418,66.418) 271 289 |
institution |
Open Polar |
collection |
Springer Nature |
op_collection_id |
crspringernat |
language |
unknown |
format |
Book Part |
author |
Kebeasy, T. R. M. Husebye, Eystein S. Hestholm, S. |
spellingShingle |
Kebeasy, T. R. M. Husebye, Eystein S. Hestholm, S. Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach |
author_facet |
Kebeasy, T. R. M. Husebye, Eystein S. Hestholm, S. |
author_sort |
Kebeasy, T. R. M. |
title |
Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach |
title_short |
Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach |
title_full |
Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach |
title_fullStr |
Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach |
title_full_unstemmed |
Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach |
title_sort |
are rock avalanches and landslides due to large earthquakes or local topographic effects? a case study of the lurøy earthquake of august 31, 1819, a 3d finite difference approach |
publisher |
Springer Netherlands |
publishDate |
2008 |
url |
http://dx.doi.org/10.1007/978-1-4020-6815-7_18 http://link.springer.com/content/pdf/10.1007/978-1-4020-6815-7_18.pdf |
long_lat |
ENVELOPE(12.849,12.849,66.418,66.418) |
geographic |
Lurøy |
geographic_facet |
Lurøy |
genre |
Lurøy |
genre_facet |
Lurøy |
op_source |
NATO Science Series: IV: Earth and Environmental Sciences Earthquake Monitoring and Seismic Hazard Mitigation in Balkan Countries page 271-289 ISSN 1568-1238 ISBN 9781402068133 9781402068157 |
op_doi |
https://doi.org/10.1007/978-1-4020-6815-7_18 |
container_start_page |
271 |
op_container_end_page |
289 |
_version_ |
1793132257462976512 |