Postglacial deformation of the Fennoscandian crust. Geophysica 33(1
Generally speaking, crustal deformation has three components, one vertical and two horizontal. This must hold true also for the Fennoscandian Shield. One of them, the vertical component, has been under intensive study for many centuries in Fennoscandia and is, therefore, relatively well-known. On th...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.513.1974 2023-05-15T16:11:45+02:00 Postglacial deformation of the Fennoscandian crust. Geophysica 33(1 Juhani Kakkuri The Pennsylvania State University CiteSeerX Archives 1997 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.513.1974 http://www.geophysica.fi/pdf/geophysica_1997_33_1_099_kakkuri.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.513.1974 http://www.geophysica.fi/pdf/geophysica_1997_33_1_099_kakkuri.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geophysica.fi/pdf/geophysica_1997_33_1_099_kakkuri.pdf Key words crustal deformation geodynamics glacial isostasy land uplift postglacial rebound text 1997 ftciteseerx 2016-01-08T09:44:52Z Generally speaking, crustal deformation has three components, one vertical and two horizontal. This must hold true also for the Fennoscandian Shield. One of them, the vertical component, has been under intensive study for many centuries in Fennoscandia and is, therefore, relatively well-known. On the contrary, only little is known of horizontal components, until now. Very recently, horizontal components of the deformation of the Fennoscandian crust have been taken under investigation, and the first results of analyses of geotechnical rock measurement, seismic, and geodetic data indicate that the maximum horizontal compression prevails in Scandinavia in the NW-SE direction. Text Fennoscandia Fennoscandian Unknown |
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ftciteseerx |
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English |
topic |
Key words crustal deformation geodynamics glacial isostasy land uplift postglacial rebound |
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Key words crustal deformation geodynamics glacial isostasy land uplift postglacial rebound Juhani Kakkuri Postglacial deformation of the Fennoscandian crust. Geophysica 33(1 |
topic_facet |
Key words crustal deformation geodynamics glacial isostasy land uplift postglacial rebound |
description |
Generally speaking, crustal deformation has three components, one vertical and two horizontal. This must hold true also for the Fennoscandian Shield. One of them, the vertical component, has been under intensive study for many centuries in Fennoscandia and is, therefore, relatively well-known. On the contrary, only little is known of horizontal components, until now. Very recently, horizontal components of the deformation of the Fennoscandian crust have been taken under investigation, and the first results of analyses of geotechnical rock measurement, seismic, and geodetic data indicate that the maximum horizontal compression prevails in Scandinavia in the NW-SE direction. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Juhani Kakkuri |
author_facet |
Juhani Kakkuri |
author_sort |
Juhani Kakkuri |
title |
Postglacial deformation of the Fennoscandian crust. Geophysica 33(1 |
title_short |
Postglacial deformation of the Fennoscandian crust. Geophysica 33(1 |
title_full |
Postglacial deformation of the Fennoscandian crust. Geophysica 33(1 |
title_fullStr |
Postglacial deformation of the Fennoscandian crust. Geophysica 33(1 |
title_full_unstemmed |
Postglacial deformation of the Fennoscandian crust. Geophysica 33(1 |
title_sort |
postglacial deformation of the fennoscandian crust. geophysica 33(1 |
publishDate |
1997 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.513.1974 http://www.geophysica.fi/pdf/geophysica_1997_33_1_099_kakkuri.pdf |
genre |
Fennoscandia Fennoscandian |
genre_facet |
Fennoscandia Fennoscandian |
op_source |
http://www.geophysica.fi/pdf/geophysica_1997_33_1_099_kakkuri.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.513.1974 http://www.geophysica.fi/pdf/geophysica_1997_33_1_099_kakkuri.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1765996930665545728 |