Late Precambrian stratigraphy and structure of the north-eastern margin of the Fennoscandian shield (East-Finnmark - Timan Region).
Later Precambrian (Riphean and Vendian) rocks occur along the north-easternb margin of the Fennoscandian Shield and the Russian Platform in Three zones: 1) the Varanger-Kildin, 2) the Timan-Kanin and 3) the Southern Barents Shelf zones. The last occupies an intermediate position and is entirely cove...
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ftnorgesgu:oai:openarchive.ngu.no:11250/2675018 2023-05-15T15:39:54+02:00 Late Precambrian stratigraphy and structure of the north-eastern margin of the Fennoscandian shield (East-Finnmark - Timan Region). Siedlecka, Anna 20352 Mun'kavarri 24363 Båtsfjord 21351 Adamsfjord 25354 Vardø VADSØ BÅTSFJORD VARDØ 1975 application/pdf https://hdl.handle.net/11250/2675018 eng eng NGU (316) https://hdl.handle.net/11250/2675018 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY 313-348 KALEDONSKE FJELLKJEDE GEOKRONOLOGI FORKASTNING STRATIGRAFI STRUKTURGEOLOGI PREKAMBRIUM Journal article 1975 ftnorgesgu 2022-07-03T15:27:18Z Later Precambrian (Riphean and Vendian) rocks occur along the north-easternb margin of the Fennoscandian Shield and the Russian Platform in Three zones: 1) the Varanger-Kildin, 2) the Timan-Kanin and 3) the Southern Barents Shelf zones. The last occupies an intermediate position and is entirely covered by the sea. Varanger-Kildin and Timan-Kanin inter-zonal sedimentary facies comparisons suggest a correlation between the miogeosynclinal sequence of the former zone and succession of strata of the Central Timans regarded as marginal miogeosynclinal in origin. The internal miogeosynclinal facies of the Timans may be expected to occur in the deep substratum of the Southern Barents Shelf while equivalents of the pericratonic deposits of the Varanger-Kildin Zone may possibly be hidden beneath the Palaeozoic strata of the Russian Platform, assuming that SW-NE margin-to-basin facies distribution constitutes a regional feature. The linear macro-facies distribution is suggested to reflect the development of NW-NE trending continental margin to the Fennoscandian Shield at the beginning of the Middle Riphean; the basin has been filled with sediments during the Middle and Upper Riphean. 36363 Article in Journal/Newspaper Båtsfjord Fennoscandian Finnmark Kildin Vadsø Varanger Vardø Finnmark NGU Open Archive (Geological Survey of Norway) Vardø ENVELOPE(31.109,31.109,70.370,70.370) Vadsø ENVELOPE(29.749,29.749,70.073,70.073) Adamsfjord ENVELOPE(26.609,26.609,70.378,70.378) |
institution |
Open Polar |
collection |
NGU Open Archive (Geological Survey of Norway) |
op_collection_id |
ftnorgesgu |
language |
English |
topic |
KALEDONSKE FJELLKJEDE GEOKRONOLOGI FORKASTNING STRATIGRAFI STRUKTURGEOLOGI PREKAMBRIUM |
spellingShingle |
KALEDONSKE FJELLKJEDE GEOKRONOLOGI FORKASTNING STRATIGRAFI STRUKTURGEOLOGI PREKAMBRIUM Siedlecka, Anna Late Precambrian stratigraphy and structure of the north-eastern margin of the Fennoscandian shield (East-Finnmark - Timan Region). |
topic_facet |
KALEDONSKE FJELLKJEDE GEOKRONOLOGI FORKASTNING STRATIGRAFI STRUKTURGEOLOGI PREKAMBRIUM |
description |
Later Precambrian (Riphean and Vendian) rocks occur along the north-easternb margin of the Fennoscandian Shield and the Russian Platform in Three zones: 1) the Varanger-Kildin, 2) the Timan-Kanin and 3) the Southern Barents Shelf zones. The last occupies an intermediate position and is entirely covered by the sea. Varanger-Kildin and Timan-Kanin inter-zonal sedimentary facies comparisons suggest a correlation between the miogeosynclinal sequence of the former zone and succession of strata of the Central Timans regarded as marginal miogeosynclinal in origin. The internal miogeosynclinal facies of the Timans may be expected to occur in the deep substratum of the Southern Barents Shelf while equivalents of the pericratonic deposits of the Varanger-Kildin Zone may possibly be hidden beneath the Palaeozoic strata of the Russian Platform, assuming that SW-NE margin-to-basin facies distribution constitutes a regional feature. The linear macro-facies distribution is suggested to reflect the development of NW-NE trending continental margin to the Fennoscandian Shield at the beginning of the Middle Riphean; the basin has been filled with sediments during the Middle and Upper Riphean. 36363 |
format |
Article in Journal/Newspaper |
author |
Siedlecka, Anna |
author_facet |
Siedlecka, Anna |
author_sort |
Siedlecka, Anna |
title |
Late Precambrian stratigraphy and structure of the north-eastern margin of the Fennoscandian shield (East-Finnmark - Timan Region). |
title_short |
Late Precambrian stratigraphy and structure of the north-eastern margin of the Fennoscandian shield (East-Finnmark - Timan Region). |
title_full |
Late Precambrian stratigraphy and structure of the north-eastern margin of the Fennoscandian shield (East-Finnmark - Timan Region). |
title_fullStr |
Late Precambrian stratigraphy and structure of the north-eastern margin of the Fennoscandian shield (East-Finnmark - Timan Region). |
title_full_unstemmed |
Late Precambrian stratigraphy and structure of the north-eastern margin of the Fennoscandian shield (East-Finnmark - Timan Region). |
title_sort |
late precambrian stratigraphy and structure of the north-eastern margin of the fennoscandian shield (east-finnmark - timan region). |
publishDate |
1975 |
url |
https://hdl.handle.net/11250/2675018 |
op_coverage |
20352 Mun'kavarri 24363 Båtsfjord 21351 Adamsfjord 25354 Vardø VADSØ BÅTSFJORD VARDØ |
long_lat |
ENVELOPE(31.109,31.109,70.370,70.370) ENVELOPE(29.749,29.749,70.073,70.073) ENVELOPE(26.609,26.609,70.378,70.378) |
geographic |
Vardø Vadsø Adamsfjord |
geographic_facet |
Vardø Vadsø Adamsfjord |
genre |
Båtsfjord Fennoscandian Finnmark Kildin Vadsø Varanger Vardø Finnmark |
genre_facet |
Båtsfjord Fennoscandian Finnmark Kildin Vadsø Varanger Vardø Finnmark |
op_source |
313-348 |
op_relation |
NGU (316) https://hdl.handle.net/11250/2675018 |
op_rights |
Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no |
op_rightsnorm |
CC-BY |
_version_ |
1766372001101905920 |