Magnetic Logs from the Lopra-1/1A and Vestmanna-1 wells (Faroe Islands)
Susceptibility results from cores (representing basalt, lapilli-tuffs and tuffs) and magnetic logs from the Lopra-1/1A well are presented. The basalts fall into a high- and a low-susceptibility group with no overlap. The high-susceptibility basalts (7 cores) have susceptibilities between 4 and 85 x...
Main Authors: | , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2006
|
Subjects: | |
Online Access: | https://pure.au.dk/portal/en/publications/a8371b20-b1f1-11db-bee9-02004c4f4f50 |
id |
ftuniaarhuspubl:oai:pure.atira.dk:publications/a8371b20-b1f1-11db-bee9-02004c4f4f50 |
---|---|
record_format |
openpolar |
spelling |
ftuniaarhuspubl:oai:pure.atira.dk:publications/a8371b20-b1f1-11db-bee9-02004c4f4f50 2024-09-15T18:05:40+00:00 Magnetic Logs from the Lopra-1/1A and Vestmanna-1 wells (Faroe Islands) Waagstein, R. Abrahamsen, N. 2006 https://pure.au.dk/portal/en/publications/a8371b20-b1f1-11db-bee9-02004c4f4f50 eng eng https://pure.au.dk/portal/en/publications/a8371b20-b1f1-11db-bee9-02004c4f4f50 info:eu-repo/semantics/restrictedAccess Waagstein , R & Abrahamsen , N 2006 , ' Magnetic Logs from the Lopra-1/1A and Vestmanna-1 wells (Faroe Islands) ' , Geological Survey of Denmark and Greenland, Bulletin , vol. 9 , pp. 41-49 . Magnetic logging rock magnetism susceptibility NRM magnetic reversals palaeomagnetism Faroe Islands Lopra Vestmanna North Atlantic article 2006 ftuniaarhuspubl 2024-07-11T05:34:28Z Susceptibility results from cores (representing basalt, lapilli-tuffs and tuffs) and magnetic logs from the Lopra-1/1A well are presented. The basalts fall into a high- and a low-susceptibility group with no overlap. The high-susceptibility basalts (7 cores) have susceptibilities between 4 and 85 x 10 -3 SI and consist of basalt with <1% vesicles from thick massive units. The low-susceptibility basalts vary from 0.6 to 1.5 x 10 -3 SI (7 cores). They are intergranular, intersertal or hypocrystalline and contain no or very little (<1%) visible magnetite, and are generally more altered than the high-susceptibility basalts. The susceptibility of 9 volcaniclastites of lapilli-tuff or tuff varies from 0.4 to 4 x 10 -3 SI. The cores reveal a bimodal distribution of magnetic susceptibily in the Lopra well. Low susceptibilities ranging from 0.4 to 4 in the well are characteristic to both altered basalts poor in magnetite, lapilli-tuffs and tuffs. Thus single measurements of susceptibility are of little use in discriminating between these three types of rock. Susceptibility logs from the Lopra-1/1A well show that the variation below 3315 m clearly distinguishes between volcaniclastics (hyaloclastites) with low and fairly constant susceptibility and basalt beds of between 5 and 10 m thickness (with high susceptibility). The volcaniclastics comprise some 60-70 % of the sequence between 3315 m and 3515 m with the maximum continuous sediment layer being 80 m thick. A 1½ m core of solid basalt at 2381 m and sidewall cores of basalt from the Lopra-1/1A well have a mean susceptibility of 22.1 ± 3.5 ´ 10 -3 SI (σ = 23.6, N = 46), while samples of hyaloclastite (lapilli-tuff and tuff) have a mean susceptibility of 0.85 ´ 10 -3 SI (σ = 0.39, N = 17). The mean values of the rock magnetic parameters for 303 basalt plugs from the Vestmanna-1 well are: Q ave = 13.3 ± 0.6 (σ = 11), S ave = 11.8 ± 0.6 ´ 10 -3 SI (σ = 11) and J ave = 4.64 ± 0.25 A/m (σ = 4.4). The polarity of the lowermost (hidden) part of the c. 4½ km thick lower ... Article in Journal/Newspaper Faroe Islands North Atlantic Vestmanna Geological Survey of Denmark and Greenland Bulletin Aarhus University: Research |
institution |
Open Polar |
collection |
Aarhus University: Research |
op_collection_id |
ftuniaarhuspubl |
language |
English |
topic |
Magnetic logging rock magnetism susceptibility NRM magnetic reversals palaeomagnetism Faroe Islands Lopra Vestmanna North Atlantic |
spellingShingle |
Magnetic logging rock magnetism susceptibility NRM magnetic reversals palaeomagnetism Faroe Islands Lopra Vestmanna North Atlantic Waagstein, R. Abrahamsen, N. Magnetic Logs from the Lopra-1/1A and Vestmanna-1 wells (Faroe Islands) |
topic_facet |
Magnetic logging rock magnetism susceptibility NRM magnetic reversals palaeomagnetism Faroe Islands Lopra Vestmanna North Atlantic |
description |
Susceptibility results from cores (representing basalt, lapilli-tuffs and tuffs) and magnetic logs from the Lopra-1/1A well are presented. The basalts fall into a high- and a low-susceptibility group with no overlap. The high-susceptibility basalts (7 cores) have susceptibilities between 4 and 85 x 10 -3 SI and consist of basalt with <1% vesicles from thick massive units. The low-susceptibility basalts vary from 0.6 to 1.5 x 10 -3 SI (7 cores). They are intergranular, intersertal or hypocrystalline and contain no or very little (<1%) visible magnetite, and are generally more altered than the high-susceptibility basalts. The susceptibility of 9 volcaniclastites of lapilli-tuff or tuff varies from 0.4 to 4 x 10 -3 SI. The cores reveal a bimodal distribution of magnetic susceptibily in the Lopra well. Low susceptibilities ranging from 0.4 to 4 in the well are characteristic to both altered basalts poor in magnetite, lapilli-tuffs and tuffs. Thus single measurements of susceptibility are of little use in discriminating between these three types of rock. Susceptibility logs from the Lopra-1/1A well show that the variation below 3315 m clearly distinguishes between volcaniclastics (hyaloclastites) with low and fairly constant susceptibility and basalt beds of between 5 and 10 m thickness (with high susceptibility). The volcaniclastics comprise some 60-70 % of the sequence between 3315 m and 3515 m with the maximum continuous sediment layer being 80 m thick. A 1½ m core of solid basalt at 2381 m and sidewall cores of basalt from the Lopra-1/1A well have a mean susceptibility of 22.1 ± 3.5 ´ 10 -3 SI (σ = 23.6, N = 46), while samples of hyaloclastite (lapilli-tuff and tuff) have a mean susceptibility of 0.85 ´ 10 -3 SI (σ = 0.39, N = 17). The mean values of the rock magnetic parameters for 303 basalt plugs from the Vestmanna-1 well are: Q ave = 13.3 ± 0.6 (σ = 11), S ave = 11.8 ± 0.6 ´ 10 -3 SI (σ = 11) and J ave = 4.64 ± 0.25 A/m (σ = 4.4). The polarity of the lowermost (hidden) part of the c. 4½ km thick lower ... |
format |
Article in Journal/Newspaper |
author |
Waagstein, R. Abrahamsen, N. |
author_facet |
Waagstein, R. Abrahamsen, N. |
author_sort |
Waagstein, R. |
title |
Magnetic Logs from the Lopra-1/1A and Vestmanna-1 wells (Faroe Islands) |
title_short |
Magnetic Logs from the Lopra-1/1A and Vestmanna-1 wells (Faroe Islands) |
title_full |
Magnetic Logs from the Lopra-1/1A and Vestmanna-1 wells (Faroe Islands) |
title_fullStr |
Magnetic Logs from the Lopra-1/1A and Vestmanna-1 wells (Faroe Islands) |
title_full_unstemmed |
Magnetic Logs from the Lopra-1/1A and Vestmanna-1 wells (Faroe Islands) |
title_sort |
magnetic logs from the lopra-1/1a and vestmanna-1 wells (faroe islands) |
publishDate |
2006 |
url |
https://pure.au.dk/portal/en/publications/a8371b20-b1f1-11db-bee9-02004c4f4f50 |
genre |
Faroe Islands North Atlantic Vestmanna Geological Survey of Denmark and Greenland Bulletin |
genre_facet |
Faroe Islands North Atlantic Vestmanna Geological Survey of Denmark and Greenland Bulletin |
op_source |
Waagstein , R & Abrahamsen , N 2006 , ' Magnetic Logs from the Lopra-1/1A and Vestmanna-1 wells (Faroe Islands) ' , Geological Survey of Denmark and Greenland, Bulletin , vol. 9 , pp. 41-49 . |
op_relation |
https://pure.au.dk/portal/en/publications/a8371b20-b1f1-11db-bee9-02004c4f4f50 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1810443196550873088 |