Syn‐deformational remanent magnetization of the Mount Eclipse Sandstone, central Australia
The palaeomagnetism of the latest Devonian‐Early Carboniferous Mount Eclipse Sandstone in central Australia reveals samples from 16 out of 31 sites having a consistent hightemperature component of natural remanent magnetization. Site‐mean directions from the two limbs of the most detailed studied sy...
Published in: | Geophysical Journal International |
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1989
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Online Access: | https://researchers.mq.edu.au/en/publications/99408d6a-9933-4b52-b2e3-735ead5a763f https://doi.org/10.1111/j.1365-246X.1989.tb02025.x http://www.scopus.com/inward/record.url?scp=0024874608&partnerID=8YFLogxK |
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ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/99408d6a-9933-4b52-b2e3-735ead5a763f 2024-05-19T07:48:39+00:00 Syn‐deformational remanent magnetization of the Mount Eclipse Sandstone, central Australia Li, Z. X. Powell, C. McA Schmidt, P. W. 1989-10-01 https://researchers.mq.edu.au/en/publications/99408d6a-9933-4b52-b2e3-735ead5a763f https://doi.org/10.1111/j.1365-246X.1989.tb02025.x http://www.scopus.com/inward/record.url?scp=0024874608&partnerID=8YFLogxK eng eng info:eu-repo/semantics/closedAccess Li , Z X , Powell , C M & Schmidt , P W 1989 , ' Syn‐deformational remanent magnetization of the Mount Eclipse Sandstone, central Australia ' , Geophysical Journal International , vol. 99 , no. 1 , pp. 205-222 . https://doi.org/10.1111/j.1365-246X.1989.tb02025.x Carboniferous Gondwanaland overprint palaeomagnetism Pangaea syndeformational article 1989 ftmacquarieunicr https://doi.org/10.1111/j.1365-246X.1989.tb02025.x 2024-04-23T02:49:45Z The palaeomagnetism of the latest Devonian‐Early Carboniferous Mount Eclipse Sandstone in central Australia reveals samples from 16 out of 31 sites having a consistent hightemperature component of natural remanent magnetization. Site‐mean directions from the two limbs of the most detailed studied syncline attain their best grouping after 75 per cent of ‘unfolding’, and further ‘unfolding’ causes a ‘cross‐over’ feature. Mineralogical studies using microscope and electron microprobe show that this remanance is most likely to be carried by secondary haematite formed by alteration of Fe‐rich minerals during the midCarboniferous deformation. Four different models are examined to reconstruct the palaeohorizontal for the syn‐deformational remanence. The best estimate of the palaeomagnetic South Pole position is lat. = 33.8°S, and long. = 121.2°E (dp = 19.2°, dm = 19.7°), close to Australia. This result indicates a rapid polarward movement of eastern Gondwanaland during the first half of the Carboniferous. We also suggest that the widespread Alice Springs Orogeny‐related overprints in central Australia were acquired during the beginning of the main phase of deformation in the mid‐Carboniferous. Article in Journal/Newspaper South pole Macquarie University Research Portal Geophysical Journal International 99 1 205 222 |
institution |
Open Polar |
collection |
Macquarie University Research Portal |
op_collection_id |
ftmacquarieunicr |
language |
English |
topic |
Carboniferous Gondwanaland overprint palaeomagnetism Pangaea syndeformational |
spellingShingle |
Carboniferous Gondwanaland overprint palaeomagnetism Pangaea syndeformational Li, Z. X. Powell, C. McA Schmidt, P. W. Syn‐deformational remanent magnetization of the Mount Eclipse Sandstone, central Australia |
topic_facet |
Carboniferous Gondwanaland overprint palaeomagnetism Pangaea syndeformational |
description |
The palaeomagnetism of the latest Devonian‐Early Carboniferous Mount Eclipse Sandstone in central Australia reveals samples from 16 out of 31 sites having a consistent hightemperature component of natural remanent magnetization. Site‐mean directions from the two limbs of the most detailed studied syncline attain their best grouping after 75 per cent of ‘unfolding’, and further ‘unfolding’ causes a ‘cross‐over’ feature. Mineralogical studies using microscope and electron microprobe show that this remanance is most likely to be carried by secondary haematite formed by alteration of Fe‐rich minerals during the midCarboniferous deformation. Four different models are examined to reconstruct the palaeohorizontal for the syn‐deformational remanence. The best estimate of the palaeomagnetic South Pole position is lat. = 33.8°S, and long. = 121.2°E (dp = 19.2°, dm = 19.7°), close to Australia. This result indicates a rapid polarward movement of eastern Gondwanaland during the first half of the Carboniferous. We also suggest that the widespread Alice Springs Orogeny‐related overprints in central Australia were acquired during the beginning of the main phase of deformation in the mid‐Carboniferous. |
format |
Article in Journal/Newspaper |
author |
Li, Z. X. Powell, C. McA Schmidt, P. W. |
author_facet |
Li, Z. X. Powell, C. McA Schmidt, P. W. |
author_sort |
Li, Z. X. |
title |
Syn‐deformational remanent magnetization of the Mount Eclipse Sandstone, central Australia |
title_short |
Syn‐deformational remanent magnetization of the Mount Eclipse Sandstone, central Australia |
title_full |
Syn‐deformational remanent magnetization of the Mount Eclipse Sandstone, central Australia |
title_fullStr |
Syn‐deformational remanent magnetization of the Mount Eclipse Sandstone, central Australia |
title_full_unstemmed |
Syn‐deformational remanent magnetization of the Mount Eclipse Sandstone, central Australia |
title_sort |
syn‐deformational remanent magnetization of the mount eclipse sandstone, central australia |
publishDate |
1989 |
url |
https://researchers.mq.edu.au/en/publications/99408d6a-9933-4b52-b2e3-735ead5a763f https://doi.org/10.1111/j.1365-246X.1989.tb02025.x http://www.scopus.com/inward/record.url?scp=0024874608&partnerID=8YFLogxK |
genre |
South pole |
genre_facet |
South pole |
op_source |
Li , Z X , Powell , C M & Schmidt , P W 1989 , ' Syn‐deformational remanent magnetization of the Mount Eclipse Sandstone, central Australia ' , Geophysical Journal International , vol. 99 , no. 1 , pp. 205-222 . https://doi.org/10.1111/j.1365-246X.1989.tb02025.x |
op_rights |
info:eu-repo/semantics/closedAccess |
op_doi |
https://doi.org/10.1111/j.1365-246X.1989.tb02025.x |
container_title |
Geophysical Journal International |
container_volume |
99 |
container_issue |
1 |
container_start_page |
205 |
op_container_end_page |
222 |
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1799466961653989376 |