Clastic dykes from the Precambrian Porsangerfjord Group, North Norway
Summary Clastic dykes are described from a late Precambrian sequence of shallow water sediments — the Porsangerfjord Group of Finnmark, North Norway. The dykes are from one stratigraphic member of the Group and only occur where this member outcrops in a zone where sedimentation was thought to have b...
Published in: | Geological Magazine |
---|---|
Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1976
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0016756800036475 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800036475 |
id |
crcambridgeupr:10.1017/s0016756800036475 |
---|---|
record_format |
openpolar |
spelling |
crcambridgeupr:10.1017/s0016756800036475 2024-05-19T07:40:14+00:00 Clastic dykes from the Precambrian Porsangerfjord Group, North Norway Williams, D. M. 1976 http://dx.doi.org/10.1017/s0016756800036475 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800036475 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 113, issue 2, page 169-176 ISSN 0016-7568 1469-5081 journal-article 1976 crcambridgeupr https://doi.org/10.1017/s0016756800036475 2024-05-02T06:50:52Z Summary Clastic dykes are described from a late Precambrian sequence of shallow water sediments — the Porsangerfjord Group of Finnmark, North Norway. The dykes are from one stratigraphic member of the Group and only occur where this member outcrops in a zone where sedimentation was thought to have been affected by recurrent earthquake shock. The dykes consist of poorly defined sandstone clasts in a muddy matrix. They exhibit no significant internal sedimentary structures. It is suggested that the dykes were intruded due to remobilization of sediment affected by a combination of tectonic shock and hydrostatic load. The dykes bear no genetic relationship to tectonic structures (cleavage and jointing) and evidence suggests that dewatering was virtually complete before the formation of the first cleavage. Article in Journal/Newspaper Finnmark North Norway Finnmark Cambridge University Press Geological Magazine 113 2 169 176 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Summary Clastic dykes are described from a late Precambrian sequence of shallow water sediments — the Porsangerfjord Group of Finnmark, North Norway. The dykes are from one stratigraphic member of the Group and only occur where this member outcrops in a zone where sedimentation was thought to have been affected by recurrent earthquake shock. The dykes consist of poorly defined sandstone clasts in a muddy matrix. They exhibit no significant internal sedimentary structures. It is suggested that the dykes were intruded due to remobilization of sediment affected by a combination of tectonic shock and hydrostatic load. The dykes bear no genetic relationship to tectonic structures (cleavage and jointing) and evidence suggests that dewatering was virtually complete before the formation of the first cleavage. |
format |
Article in Journal/Newspaper |
author |
Williams, D. M. |
spellingShingle |
Williams, D. M. Clastic dykes from the Precambrian Porsangerfjord Group, North Norway |
author_facet |
Williams, D. M. |
author_sort |
Williams, D. M. |
title |
Clastic dykes from the Precambrian Porsangerfjord Group, North Norway |
title_short |
Clastic dykes from the Precambrian Porsangerfjord Group, North Norway |
title_full |
Clastic dykes from the Precambrian Porsangerfjord Group, North Norway |
title_fullStr |
Clastic dykes from the Precambrian Porsangerfjord Group, North Norway |
title_full_unstemmed |
Clastic dykes from the Precambrian Porsangerfjord Group, North Norway |
title_sort |
clastic dykes from the precambrian porsangerfjord group, north norway |
publisher |
Cambridge University Press (CUP) |
publishDate |
1976 |
url |
http://dx.doi.org/10.1017/s0016756800036475 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800036475 |
genre |
Finnmark North Norway Finnmark |
genre_facet |
Finnmark North Norway Finnmark |
op_source |
Geological Magazine volume 113, issue 2, page 169-176 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800036475 |
container_title |
Geological Magazine |
container_volume |
113 |
container_issue |
2 |
container_start_page |
169 |
op_container_end_page |
176 |
_version_ |
1799479816241545216 |