Boudinage-type Structures at Sørfinnset, Gildeskaal, North Norway
Abstract A layer of massive and lineated hornblende-biotite-gneiss has fractured along ac -joints (perpendicular to the layering and b –lineation), at regular intervals along its lower surface in contact with a thin marble bed. The joints have been opened from below and the marble has penetrated upw...
Published in: | Geological Magazine |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Cambridge University Press (CUP)
1964
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Online Access: | http://dx.doi.org/10.1017/s0016756800050020 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800050020 |
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crcambridgeupr:10.1017/s0016756800050020 2024-03-03T08:47:13+00:00 Boudinage-type Structures at Sørfinnset, Gildeskaal, North Norway Bradshaw, R. Wells, M. K. 1964 http://dx.doi.org/10.1017/s0016756800050020 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800050020 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 101, issue 6, page 488-495 ISSN 0016-7568 1469-5081 Geology journal-article 1964 crcambridgeupr https://doi.org/10.1017/s0016756800050020 2024-02-08T08:32:46Z Abstract A layer of massive and lineated hornblende-biotite-gneiss has fractured along ac -joints (perpendicular to the layering and b –lineation), at regular intervals along its lower surface in contact with a thin marble bed. The joints have been opened from below and the marble has penetrated upwards to form intrusive tongues caused by extremely plastic flow folding, as shown by the unbroken banding in the marble. The structure constitutes a variety of one-sided boudinage involving segmentation in the lowest metre or so of the hornblendic rock, while the extreme marble deformation is all accommodated in a few centimetres thickness. The structures must have developed at relatively high temperatures to allow contemporaneous segregation of quartz-feldspar pegmatite veins from the hornblendic rock, and of diopside reaction skarns at the marble junctions. Article in Journal/Newspaper North Norway Cambridge University Press Norway Sørfinnset ENVELOPE(13.983,13.983,66.978,66.978) Geological Magazine 101 6 488 495 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Geology |
spellingShingle |
Geology Bradshaw, R. Wells, M. K. Boudinage-type Structures at Sørfinnset, Gildeskaal, North Norway |
topic_facet |
Geology |
description |
Abstract A layer of massive and lineated hornblende-biotite-gneiss has fractured along ac -joints (perpendicular to the layering and b –lineation), at regular intervals along its lower surface in contact with a thin marble bed. The joints have been opened from below and the marble has penetrated upwards to form intrusive tongues caused by extremely plastic flow folding, as shown by the unbroken banding in the marble. The structure constitutes a variety of one-sided boudinage involving segmentation in the lowest metre or so of the hornblendic rock, while the extreme marble deformation is all accommodated in a few centimetres thickness. The structures must have developed at relatively high temperatures to allow contemporaneous segregation of quartz-feldspar pegmatite veins from the hornblendic rock, and of diopside reaction skarns at the marble junctions. |
format |
Article in Journal/Newspaper |
author |
Bradshaw, R. Wells, M. K. |
author_facet |
Bradshaw, R. Wells, M. K. |
author_sort |
Bradshaw, R. |
title |
Boudinage-type Structures at Sørfinnset, Gildeskaal, North Norway |
title_short |
Boudinage-type Structures at Sørfinnset, Gildeskaal, North Norway |
title_full |
Boudinage-type Structures at Sørfinnset, Gildeskaal, North Norway |
title_fullStr |
Boudinage-type Structures at Sørfinnset, Gildeskaal, North Norway |
title_full_unstemmed |
Boudinage-type Structures at Sørfinnset, Gildeskaal, North Norway |
title_sort |
boudinage-type structures at sørfinnset, gildeskaal, north norway |
publisher |
Cambridge University Press (CUP) |
publishDate |
1964 |
url |
http://dx.doi.org/10.1017/s0016756800050020 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800050020 |
long_lat |
ENVELOPE(13.983,13.983,66.978,66.978) |
geographic |
Norway Sørfinnset |
geographic_facet |
Norway Sørfinnset |
genre |
North Norway |
genre_facet |
North Norway |
op_source |
Geological Magazine volume 101, issue 6, page 488-495 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800050020 |
container_title |
Geological Magazine |
container_volume |
101 |
container_issue |
6 |
container_start_page |
488 |
op_container_end_page |
495 |
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1792503375958376448 |