Late Precambrian and Cambro-Ordovician sedimentation in East Finnmark.
The presence of two closely spaced tillite formations within the Precambrian and Cambro-Ordovician sediments of eastern Finnmark permits subdivision into pre-glacial and post-glacial regimes. On the northern side of Varangerfjord the preglacial \"Older Sandstone Series\" of Precambrian age...
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ftnorgesgu:oai:openarchive.ngu.no:11250/2674937 2023-05-15T16:13:36+02:00 Late Precambrian and Cambro-Ordovician sedimentation in East Finnmark. Hobday, D.A. Reading, H.G. Banks, N. L. Edwards, M.B. Geddes, W.P. TANA LEBESBY PORSANGER 20352 Mun'kavarri 21352 Ul'lugai'sa 22362 Langfjorden 24353 Vadsø 1971 application/pdf https://hdl.handle.net/11250/2674937 eng eng NGU (269) https://hdl.handle.net/11250/2674937 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY 197-236 GLASIALGEOLOGI PETROGRAFI STRATIGRAFI SEDIMENTOLOGI FACIES Journal article 1971 ftnorgesgu 2022-07-03T15:26:52Z The presence of two closely spaced tillite formations within the Precambrian and Cambro-Ordovician sediments of eastern Finnmark permits subdivision into pre-glacial and post-glacial regimes. On the northern side of Varangerfjord the preglacial \"Older Sandstone Series\" of Precambrian age consists of six lithological members, which collectively represent transgressive-regressive cycles. Within each cycle shallow marine siltstones are overlain by coarser sediments of intertidal, estuarine and fluvial origin. Two distinct sedimentary sources are suggested by palaeocurrent and petrographic evidence. Influx from a westerly direction tended to dominate over a volumetrically less significant source of immature detritus from the east or southeast. The \"Older Sandstone Series\" is overlain with slight angular unconformity by the glacially dominated sediments of the lower part of the Vestertana Group. The two tillite formations consists of both continental and marine glacial deposits, with marine influence increasing northward. The interglacial Nyborg Formation consists largely of turbidite sandstones, with a transgressive sequence at the base and a regressive sequence at the top. All of the sediments of glacially dominated regime appear to have been derived from the south. 35121 Article in Journal/Newspaper Finnmark Lebesby Porsanger Tana Vadsø Varangerfjord Varangerfjord* Finnmark NGU Open Archive (Geological Survey of Norway) Porsanger ENVELOPE(24.956,24.956,70.052,70.052) Vadsø ENVELOPE(29.749,29.749,70.073,70.073) Vestertana ENVELOPE(27.868,27.868,70.424,70.424) Lebesby ENVELOPE(27.002,27.002,70.573,70.573) Langfjorden ENVELOPE(12.676,12.676,65.378,65.378) |
institution |
Open Polar |
collection |
NGU Open Archive (Geological Survey of Norway) |
op_collection_id |
ftnorgesgu |
language |
English |
topic |
GLASIALGEOLOGI PETROGRAFI STRATIGRAFI SEDIMENTOLOGI FACIES |
spellingShingle |
GLASIALGEOLOGI PETROGRAFI STRATIGRAFI SEDIMENTOLOGI FACIES Hobday, D.A. Reading, H.G. Banks, N. L. Edwards, M.B. Geddes, W.P. Late Precambrian and Cambro-Ordovician sedimentation in East Finnmark. |
topic_facet |
GLASIALGEOLOGI PETROGRAFI STRATIGRAFI SEDIMENTOLOGI FACIES |
description |
The presence of two closely spaced tillite formations within the Precambrian and Cambro-Ordovician sediments of eastern Finnmark permits subdivision into pre-glacial and post-glacial regimes. On the northern side of Varangerfjord the preglacial \"Older Sandstone Series\" of Precambrian age consists of six lithological members, which collectively represent transgressive-regressive cycles. Within each cycle shallow marine siltstones are overlain by coarser sediments of intertidal, estuarine and fluvial origin. Two distinct sedimentary sources are suggested by palaeocurrent and petrographic evidence. Influx from a westerly direction tended to dominate over a volumetrically less significant source of immature detritus from the east or southeast. The \"Older Sandstone Series\" is overlain with slight angular unconformity by the glacially dominated sediments of the lower part of the Vestertana Group. The two tillite formations consists of both continental and marine glacial deposits, with marine influence increasing northward. The interglacial Nyborg Formation consists largely of turbidite sandstones, with a transgressive sequence at the base and a regressive sequence at the top. All of the sediments of glacially dominated regime appear to have been derived from the south. 35121 |
format |
Article in Journal/Newspaper |
author |
Hobday, D.A. Reading, H.G. Banks, N. L. Edwards, M.B. Geddes, W.P. |
author_facet |
Hobday, D.A. Reading, H.G. Banks, N. L. Edwards, M.B. Geddes, W.P. |
author_sort |
Hobday, D.A. |
title |
Late Precambrian and Cambro-Ordovician sedimentation in East Finnmark. |
title_short |
Late Precambrian and Cambro-Ordovician sedimentation in East Finnmark. |
title_full |
Late Precambrian and Cambro-Ordovician sedimentation in East Finnmark. |
title_fullStr |
Late Precambrian and Cambro-Ordovician sedimentation in East Finnmark. |
title_full_unstemmed |
Late Precambrian and Cambro-Ordovician sedimentation in East Finnmark. |
title_sort |
late precambrian and cambro-ordovician sedimentation in east finnmark. |
publishDate |
1971 |
url |
https://hdl.handle.net/11250/2674937 |
op_coverage |
TANA LEBESBY PORSANGER 20352 Mun'kavarri 21352 Ul'lugai'sa 22362 Langfjorden 24353 Vadsø |
long_lat |
ENVELOPE(24.956,24.956,70.052,70.052) ENVELOPE(29.749,29.749,70.073,70.073) ENVELOPE(27.868,27.868,70.424,70.424) ENVELOPE(27.002,27.002,70.573,70.573) ENVELOPE(12.676,12.676,65.378,65.378) |
geographic |
Porsanger Vadsø Vestertana Lebesby Langfjorden |
geographic_facet |
Porsanger Vadsø Vestertana Lebesby Langfjorden |
genre |
Finnmark Lebesby Porsanger Tana Vadsø Varangerfjord Varangerfjord* Finnmark |
genre_facet |
Finnmark Lebesby Porsanger Tana Vadsø Varangerfjord Varangerfjord* Finnmark |
op_source |
197-236 |
op_relation |
NGU (269) https://hdl.handle.net/11250/2674937 |
op_rights |
Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no |
op_rightsnorm |
CC-BY |
_version_ |
1765999383111794688 |