Seismotectonics and lithospheric stresses in the northern Fennoscandian shield
The seismicity, fault distribution and stress pattern of northern Fennoscandia are investigated. Some active fault zones are suggested, eg several faults exposed to large displacement at the late-glacial phase about 9000 yr ago. Stress orientations, derived from crack distribution and a few earthqua...
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ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_232478 2023-05-15T16:11:43+02:00 Seismotectonics and lithospheric stresses in the northern Fennoscandian shield Wahlström, R. Assinovskaya, B. 1998 https://gfzpublic.gfz-potsdam.de/pubman/item/item_232478 unknown https://gfzpublic.gfz-potsdam.de/pubman/item/item_232478 Geophysica 550 - Earth sciences info:eu-repo/semantics/article 1998 ftgfzpotsdam 2022-09-14T05:56:44Z The seismicity, fault distribution and stress pattern of northern Fennoscandia are investigated. Some active fault zones are suggested, eg several faults exposed to large displacement at the late-glacial phase about 9000 yr ago. Stress orientations, derived from crack distribution and a few earthquake focal-mechanism solutions, are different in different areas. In some cases there is a good agreement with expectations from ridge-push generated and propagated compressive stress. Hoever, the inhomogeneity in the stress field of the region as a whole indicates contribution from local factors. Article in Journal/Newspaper Fennoscandia Fennoscandian GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
institution |
Open Polar |
collection |
GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
op_collection_id |
ftgfzpotsdam |
language |
unknown |
topic |
550 - Earth sciences |
spellingShingle |
550 - Earth sciences Wahlström, R. Assinovskaya, B. Seismotectonics and lithospheric stresses in the northern Fennoscandian shield |
topic_facet |
550 - Earth sciences |
description |
The seismicity, fault distribution and stress pattern of northern Fennoscandia are investigated. Some active fault zones are suggested, eg several faults exposed to large displacement at the late-glacial phase about 9000 yr ago. Stress orientations, derived from crack distribution and a few earthquake focal-mechanism solutions, are different in different areas. In some cases there is a good agreement with expectations from ridge-push generated and propagated compressive stress. Hoever, the inhomogeneity in the stress field of the region as a whole indicates contribution from local factors. |
format |
Article in Journal/Newspaper |
author |
Wahlström, R. Assinovskaya, B. |
author_facet |
Wahlström, R. Assinovskaya, B. |
author_sort |
Wahlström, R. |
title |
Seismotectonics and lithospheric stresses in the northern Fennoscandian shield |
title_short |
Seismotectonics and lithospheric stresses in the northern Fennoscandian shield |
title_full |
Seismotectonics and lithospheric stresses in the northern Fennoscandian shield |
title_fullStr |
Seismotectonics and lithospheric stresses in the northern Fennoscandian shield |
title_full_unstemmed |
Seismotectonics and lithospheric stresses in the northern Fennoscandian shield |
title_sort |
seismotectonics and lithospheric stresses in the northern fennoscandian shield |
publishDate |
1998 |
url |
https://gfzpublic.gfz-potsdam.de/pubman/item/item_232478 |
genre |
Fennoscandia Fennoscandian |
genre_facet |
Fennoscandia Fennoscandian |
op_source |
Geophysica |
op_relation |
https://gfzpublic.gfz-potsdam.de/pubman/item/item_232478 |
_version_ |
1765996882047270912 |