How stress transfer between volcanic and seismic zones affects volcanic and earthquake
Oceanic transform faults and ridge segments form a network where mechanical interaction is to be expected. In particular, dike emplacement in ridge segments is likely to affect earthquake activity in the adjacent transform faults through processes such as stress transfer. Similarly, strike-slip disp...
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ftdatacite:10.23689/fidgeo-1854 2023-05-15T16:48:51+02:00 How stress transfer between volcanic and seismic zones affects volcanic and earthquake Gudmundsson, Agust Philipp, Sonja L. 2006 https://dx.doi.org/10.23689/fidgeo-1854 https://e-docs.geo-leo.de/handle/11858/00-1735-0000-0001-343F-D de ger Universitätsverlag Göttingen Text Article article-journal ScholarlyArticle 2006 ftdatacite https://doi.org/10.23689/fidgeo-1854 2021-11-05T12:55:41Z Oceanic transform faults and ridge segments form a network where mechanical interaction is to be expected. In particular, dike emplacement in ridge segments is likely to affect earthquake activity in the adjacent transform faults through processes such as stress transfer. Similarly, strike-slip displacement across transform faults may trigger dike injections and, eventually, eruptions in the adjacent ridge segments. For obvious reasons, direct observations of the possible mechanical interaction between submarine transform zones and ridge segments at mid-ocean ridges are difficult. The subaerial seismic zones of Iceland, however, are in clear spatial connections with the adjacent volcanic zones. These zones, therefore, provide excellent opportunities to study stress transfer between volcanic and seismic zones (Gudmundsson 2000)... : conference Text Iceland DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
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German |
description |
Oceanic transform faults and ridge segments form a network where mechanical interaction is to be expected. In particular, dike emplacement in ridge segments is likely to affect earthquake activity in the adjacent transform faults through processes such as stress transfer. Similarly, strike-slip displacement across transform faults may trigger dike injections and, eventually, eruptions in the adjacent ridge segments. For obvious reasons, direct observations of the possible mechanical interaction between submarine transform zones and ridge segments at mid-ocean ridges are difficult. The subaerial seismic zones of Iceland, however, are in clear spatial connections with the adjacent volcanic zones. These zones, therefore, provide excellent opportunities to study stress transfer between volcanic and seismic zones (Gudmundsson 2000)... : conference |
format |
Text |
author |
Gudmundsson, Agust Philipp, Sonja L. |
spellingShingle |
Gudmundsson, Agust Philipp, Sonja L. How stress transfer between volcanic and seismic zones affects volcanic and earthquake |
author_facet |
Gudmundsson, Agust Philipp, Sonja L. |
author_sort |
Gudmundsson, Agust |
title |
How stress transfer between volcanic and seismic zones affects volcanic and earthquake |
title_short |
How stress transfer between volcanic and seismic zones affects volcanic and earthquake |
title_full |
How stress transfer between volcanic and seismic zones affects volcanic and earthquake |
title_fullStr |
How stress transfer between volcanic and seismic zones affects volcanic and earthquake |
title_full_unstemmed |
How stress transfer between volcanic and seismic zones affects volcanic and earthquake |
title_sort |
how stress transfer between volcanic and seismic zones affects volcanic and earthquake |
publisher |
Universitätsverlag Göttingen |
publishDate |
2006 |
url |
https://dx.doi.org/10.23689/fidgeo-1854 https://e-docs.geo-leo.de/handle/11858/00-1735-0000-0001-343F-D |
genre |
Iceland |
genre_facet |
Iceland |
op_doi |
https://doi.org/10.23689/fidgeo-1854 |
_version_ |
1766038938656440320 |