Pseudotachylit fra de kaledonske skyvesoner i Jotunheimens forgårder, Gudbrandsdalen, og deres dannelsesbetingelser
The old tourists thought of the district as an anterior court to the Jotunheim mountainrange, and this designation also applies in a geological sense. We here find exposed the basement parts in front of the heavy thrust- masses which advanced from the NW during the 3rd of the 3 distinct periods of C...
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ftnorgesgu:oai:openarchive.ngu.no:11250/2674607 2023-05-15T18:29:47+02:00 Pseudotachylit fra de kaledonske skyvesoner i Jotunheimens forgårder, Gudbrandsdalen, og deres dannelsesbetingelser Dietrichson, Brynjulf 1953 application/pdf https://hdl.handle.net/11250/2674607 nor nor NGU (184) https://hdl.handle.net/11250/2674607 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY 23-70 + p PETROGRAFI STØRKNINGSBERGART OMDANNET BERGART SEDIMENTÆR BERGART ANORTOSITT GRANITT Journal article 1953 ftnorgesgu 2022-07-03T15:26:31Z The old tourists thought of the district as an anterior court to the Jotunheim mountainrange, and this designation also applies in a geological sense. We here find exposed the basement parts in front of the heavy thrust- masses which advanced from the NW during the 3rd of the 3 distinct periods of Caledonian orogeny pointed out in our district and probably corresponding to: 1. The Trondheim orogeny, 2. The Ekne orogeny, 3. The Svalbard orogeny (Th. Vogt 1928). The second period is characterized by succsessive folding, overfolding and imbrication advancing from NE(SSW) with axes NW(WNW) to SE (ESE), particulary distinct impressed in the topography of our district as appears from the map fig. 1. The pseudotachylites and the supposition for their genesis are considered by prominent geologists in this country and abroad (Goldschmidt and Holmes) as most puzzeling. 35542 Article in Journal/Newspaper Svalbard NGU Open Archive (Geological Survey of Norway) Jotunheim ENVELOPE(-22.583,-22.583,75.267,75.267) Svalbard |
institution |
Open Polar |
collection |
NGU Open Archive (Geological Survey of Norway) |
op_collection_id |
ftnorgesgu |
language |
Norwegian |
topic |
PETROGRAFI STØRKNINGSBERGART OMDANNET BERGART SEDIMENTÆR BERGART ANORTOSITT GRANITT |
spellingShingle |
PETROGRAFI STØRKNINGSBERGART OMDANNET BERGART SEDIMENTÆR BERGART ANORTOSITT GRANITT Dietrichson, Brynjulf Pseudotachylit fra de kaledonske skyvesoner i Jotunheimens forgårder, Gudbrandsdalen, og deres dannelsesbetingelser |
topic_facet |
PETROGRAFI STØRKNINGSBERGART OMDANNET BERGART SEDIMENTÆR BERGART ANORTOSITT GRANITT |
description |
The old tourists thought of the district as an anterior court to the Jotunheim mountainrange, and this designation also applies in a geological sense. We here find exposed the basement parts in front of the heavy thrust- masses which advanced from the NW during the 3rd of the 3 distinct periods of Caledonian orogeny pointed out in our district and probably corresponding to: 1. The Trondheim orogeny, 2. The Ekne orogeny, 3. The Svalbard orogeny (Th. Vogt 1928). The second period is characterized by succsessive folding, overfolding and imbrication advancing from NE(SSW) with axes NW(WNW) to SE (ESE), particulary distinct impressed in the topography of our district as appears from the map fig. 1. The pseudotachylites and the supposition for their genesis are considered by prominent geologists in this country and abroad (Goldschmidt and Holmes) as most puzzeling. 35542 |
format |
Article in Journal/Newspaper |
author |
Dietrichson, Brynjulf |
author_facet |
Dietrichson, Brynjulf |
author_sort |
Dietrichson, Brynjulf |
title |
Pseudotachylit fra de kaledonske skyvesoner i Jotunheimens forgårder, Gudbrandsdalen, og deres dannelsesbetingelser |
title_short |
Pseudotachylit fra de kaledonske skyvesoner i Jotunheimens forgårder, Gudbrandsdalen, og deres dannelsesbetingelser |
title_full |
Pseudotachylit fra de kaledonske skyvesoner i Jotunheimens forgårder, Gudbrandsdalen, og deres dannelsesbetingelser |
title_fullStr |
Pseudotachylit fra de kaledonske skyvesoner i Jotunheimens forgårder, Gudbrandsdalen, og deres dannelsesbetingelser |
title_full_unstemmed |
Pseudotachylit fra de kaledonske skyvesoner i Jotunheimens forgårder, Gudbrandsdalen, og deres dannelsesbetingelser |
title_sort |
pseudotachylit fra de kaledonske skyvesoner i jotunheimens forgårder, gudbrandsdalen, og deres dannelsesbetingelser |
publishDate |
1953 |
url |
https://hdl.handle.net/11250/2674607 |
long_lat |
ENVELOPE(-22.583,-22.583,75.267,75.267) |
geographic |
Jotunheim Svalbard |
geographic_facet |
Jotunheim Svalbard |
genre |
Svalbard |
genre_facet |
Svalbard |
op_source |
23-70 + p |
op_relation |
NGU (184) https://hdl.handle.net/11250/2674607 |
op_rights |
Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no |
op_rightsnorm |
CC-BY |
_version_ |
1766213157859098624 |