Palaeointensity and palaeomagnetic study of Cretaceous and Palaeocene rocks from Western Antarctica
A combined palaeodirectional and palaeointensity study of a representative collection of plutonic rocks from the Antarctic Peninsula batholith from the western part of the Antarctic Peninsula, near the Ukrainian Antarctic base 'Academik Vernadsky' were carried out. Petrographically, the co...
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fthighwire:oai:open-archive.highwire.org:gji:189/1/204 2023-05-15T13:59:18+02:00 Palaeointensity and palaeomagnetic study of Cretaceous and Palaeocene rocks from Western Antarctica Shcherbakova, V. V. Bakhmutov, V. G. Shcherbakov, V. P. Zhidkov, G. V. Shpyra, V. V. 2012-04-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/189/1/204 https://doi.org/10.1111/j.1365-246X.2012.05357.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/189/1/204 http://dx.doi.org/10.1111/j.1365-246X.2012.05357.x Copyright (C) 2012, Oxford University Press Geomagnetism rock magnetism and palaeomagnetism TEXT 2012 fthighwire https://doi.org/10.1111/j.1365-246X.2012.05357.x 2015-02-28T17:33:45Z A combined palaeodirectional and palaeointensity study of a representative collection of plutonic rocks from the Antarctic Peninsula batholith from the western part of the Antarctic Peninsula, near the Ukrainian Antarctic base 'Academik Vernadsky' were carried out. Petrographically, the collection includes gabbros, diorites and quartz diorites, tonalities, granodiorites and granites. The ages of igneous complex emplacement vary from 50 to 117 Ma with most of the rocks belonging to the Cretaceous Normal Superchron. The characteristic remanent magnetizations were isolated by stepwise thermal demagnetization over the temperature interval 440-590°C and their intensities amount to 95 per cent of the NRM. The geographic positions of palaeopoles do not contradict the ‘key poles’ of the Antarctic Peninsula between 90 and 60 Ma. A significant part of the collection was subjected to Coe-modified Thellier palaeointensity experiments with the pTRM checks, which yielded seven reliable palaeointensity determinations for seven different locations. The obtained VDMs are relatively low for all sites, being on average about half of the present day VDM. The analysis of available palaeointensity data for the Cretaceous, Miocene and Middle Jurassic indicates the existence of strong correlations between the mean VDM and VDM scatter versus the rate of reversals. However, due to the shortage of data, the correlations are not significant at the 5 per cent significance level. Text Antarc* Antarctic Antarctic Peninsula Antarctica HighWire Press (Stanford University) Antarctic Antarctic Peninsula The Antarctic Geophysical Journal International 189 1 204 228 |
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Open Polar |
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HighWire Press (Stanford University) |
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fthighwire |
language |
English |
topic |
Geomagnetism rock magnetism and palaeomagnetism |
spellingShingle |
Geomagnetism rock magnetism and palaeomagnetism Shcherbakova, V. V. Bakhmutov, V. G. Shcherbakov, V. P. Zhidkov, G. V. Shpyra, V. V. Palaeointensity and palaeomagnetic study of Cretaceous and Palaeocene rocks from Western Antarctica |
topic_facet |
Geomagnetism rock magnetism and palaeomagnetism |
description |
A combined palaeodirectional and palaeointensity study of a representative collection of plutonic rocks from the Antarctic Peninsula batholith from the western part of the Antarctic Peninsula, near the Ukrainian Antarctic base 'Academik Vernadsky' were carried out. Petrographically, the collection includes gabbros, diorites and quartz diorites, tonalities, granodiorites and granites. The ages of igneous complex emplacement vary from 50 to 117 Ma with most of the rocks belonging to the Cretaceous Normal Superchron. The characteristic remanent magnetizations were isolated by stepwise thermal demagnetization over the temperature interval 440-590°C and their intensities amount to 95 per cent of the NRM. The geographic positions of palaeopoles do not contradict the ‘key poles’ of the Antarctic Peninsula between 90 and 60 Ma. A significant part of the collection was subjected to Coe-modified Thellier palaeointensity experiments with the pTRM checks, which yielded seven reliable palaeointensity determinations for seven different locations. The obtained VDMs are relatively low for all sites, being on average about half of the present day VDM. The analysis of available palaeointensity data for the Cretaceous, Miocene and Middle Jurassic indicates the existence of strong correlations between the mean VDM and VDM scatter versus the rate of reversals. However, due to the shortage of data, the correlations are not significant at the 5 per cent significance level. |
format |
Text |
author |
Shcherbakova, V. V. Bakhmutov, V. G. Shcherbakov, V. P. Zhidkov, G. V. Shpyra, V. V. |
author_facet |
Shcherbakova, V. V. Bakhmutov, V. G. Shcherbakov, V. P. Zhidkov, G. V. Shpyra, V. V. |
author_sort |
Shcherbakova, V. V. |
title |
Palaeointensity and palaeomagnetic study of Cretaceous and Palaeocene rocks from Western Antarctica |
title_short |
Palaeointensity and palaeomagnetic study of Cretaceous and Palaeocene rocks from Western Antarctica |
title_full |
Palaeointensity and palaeomagnetic study of Cretaceous and Palaeocene rocks from Western Antarctica |
title_fullStr |
Palaeointensity and palaeomagnetic study of Cretaceous and Palaeocene rocks from Western Antarctica |
title_full_unstemmed |
Palaeointensity and palaeomagnetic study of Cretaceous and Palaeocene rocks from Western Antarctica |
title_sort |
palaeointensity and palaeomagnetic study of cretaceous and palaeocene rocks from western antarctica |
publisher |
Oxford University Press |
publishDate |
2012 |
url |
http://gji.oxfordjournals.org/cgi/content/short/189/1/204 https://doi.org/10.1111/j.1365-246X.2012.05357.x |
geographic |
Antarctic Antarctic Peninsula The Antarctic |
geographic_facet |
Antarctic Antarctic Peninsula The Antarctic |
genre |
Antarc* Antarctic Antarctic Peninsula Antarctica |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Antarctica |
op_relation |
http://gji.oxfordjournals.org/cgi/content/short/189/1/204 http://dx.doi.org/10.1111/j.1365-246X.2012.05357.x |
op_rights |
Copyright (C) 2012, Oxford University Press |
op_doi |
https://doi.org/10.1111/j.1365-246X.2012.05357.x |
container_title |
Geophysical Journal International |
container_volume |
189 |
container_issue |
1 |
container_start_page |
204 |
op_container_end_page |
228 |
_version_ |
1766267847139393536 |