Palaeomagnetism of Red Beds of the Late Devonian Worange Point Formation, Se Australia
Gently folded strata of the Late Devonian Merrimbula Group along the south coast of New South Wales are similar to numerous deposits of Late Devonian to Early Carboniferous, subaerial to shallow marine, quartzose sandstone that are known as the Lambie Facies of SE Australia. Because the Lambie sands...
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ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/28367a5f-0ad5-413d-9e8b-43313877d3af 2023-05-15T18:23:16+02:00 Palaeomagnetism of Red Beds of the Late Devonian Worange Point Formation, Se Australia Thrupp, G. A. Kent, D. V. Schmidt, P. W. Powell, C. Mca 1991 https://researchers.mq.edu.au/en/publications/28367a5f-0ad5-413d-9e8b-43313877d3af https://doi.org/10.1111/j.1365-246X.1991.tb02503.x http://www.scopus.com/inward/record.url?scp=0026053178&partnerID=8YFLogxK eng eng info:eu-repo/semantics/restrictedAccess Thrupp , G A , Kent , D V , Schmidt , P W & Powell , C M 1991 , ' Palaeomagnetism of Red Beds of the Late Devonian Worange Point Formation, Se Australia ' , Geophysical Journal International , vol. 104 , no. 1 , pp. 179-202 . https://doi.org/10.1111/j.1365-246X.1991.tb02503.x article 1991 ftmacquarieunicr https://doi.org/10.1111/j.1365-246X.1991.tb02503.x 2022-11-27T12:09:49Z Gently folded strata of the Late Devonian Merrimbula Group along the south coast of New South Wales are similar to numerous deposits of Late Devonian to Early Carboniferous, subaerial to shallow marine, quartzose sandstone that are known as the Lambie Facies of SE Australia. Because the Lambie sands overlap the early Palaeozoic tectonic elements of the Lachlan Fold Belt, large displacement since the Late Devonian of any Lachlan terranes, with respect to interior Australia, is precluded. We collected oriented core samples from 37 sites primarily in reddish, quartzose litharenites of the Worange Point Formation. the remanent magnetization is carried by haematite. Incremental thermal demagnetization reveals a dominant, well‐defined, steep‐upward‐north component of magnetization that post‐dates the mid‐Carboniferous folding. the south pole position (146.4°E, 68.6°S, A95 3.1°) derived from the overprinted specimens is close to both the Late Carboniferous and mid‐Cretaceous reference poles as well as the spin axis of today. the overprint is attributed to both viscous partial thermoremanent and chemical remanent magnetization (VPTRM and CRM). Its exclusively normal polarity is consistent with a mid‐Cretaceous acquisition, perhaps related to the rifting of the SE Australian margin. A characteristic component of magnetization is isolated between ‐660° and ‐680°C in ‐30 per cent of the samples. Although a regional fold test of the overall result is inconclusive because the directions of characteristic magnetization are generally close to the axes of folding, two sets of samples from opposite limbs of a local syncline pass a fold test at 90 per cent confidence, indicating a pre‐folding origin of the remanence. the presence of both polarities in thin horizons, some of which are palaeosols, and diagenetic haematite associated with incipient cleavage formed in an early stage of deformation before folding, indicates that the acquisition of remanent magnetization occurred over a protracted period. an analysis that combines ... Article in Journal/Newspaper South pole Macquarie University Research Portal South Pole Geophysical Journal International 104 1 179 202 |
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Open Polar |
collection |
Macquarie University Research Portal |
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ftmacquarieunicr |
language |
English |
description |
Gently folded strata of the Late Devonian Merrimbula Group along the south coast of New South Wales are similar to numerous deposits of Late Devonian to Early Carboniferous, subaerial to shallow marine, quartzose sandstone that are known as the Lambie Facies of SE Australia. Because the Lambie sands overlap the early Palaeozoic tectonic elements of the Lachlan Fold Belt, large displacement since the Late Devonian of any Lachlan terranes, with respect to interior Australia, is precluded. We collected oriented core samples from 37 sites primarily in reddish, quartzose litharenites of the Worange Point Formation. the remanent magnetization is carried by haematite. Incremental thermal demagnetization reveals a dominant, well‐defined, steep‐upward‐north component of magnetization that post‐dates the mid‐Carboniferous folding. the south pole position (146.4°E, 68.6°S, A95 3.1°) derived from the overprinted specimens is close to both the Late Carboniferous and mid‐Cretaceous reference poles as well as the spin axis of today. the overprint is attributed to both viscous partial thermoremanent and chemical remanent magnetization (VPTRM and CRM). Its exclusively normal polarity is consistent with a mid‐Cretaceous acquisition, perhaps related to the rifting of the SE Australian margin. A characteristic component of magnetization is isolated between ‐660° and ‐680°C in ‐30 per cent of the samples. Although a regional fold test of the overall result is inconclusive because the directions of characteristic magnetization are generally close to the axes of folding, two sets of samples from opposite limbs of a local syncline pass a fold test at 90 per cent confidence, indicating a pre‐folding origin of the remanence. the presence of both polarities in thin horizons, some of which are palaeosols, and diagenetic haematite associated with incipient cleavage formed in an early stage of deformation before folding, indicates that the acquisition of remanent magnetization occurred over a protracted period. an analysis that combines ... |
format |
Article in Journal/Newspaper |
author |
Thrupp, G. A. Kent, D. V. Schmidt, P. W. Powell, C. Mca |
spellingShingle |
Thrupp, G. A. Kent, D. V. Schmidt, P. W. Powell, C. Mca Palaeomagnetism of Red Beds of the Late Devonian Worange Point Formation, Se Australia |
author_facet |
Thrupp, G. A. Kent, D. V. Schmidt, P. W. Powell, C. Mca |
author_sort |
Thrupp, G. A. |
title |
Palaeomagnetism of Red Beds of the Late Devonian Worange Point Formation, Se Australia |
title_short |
Palaeomagnetism of Red Beds of the Late Devonian Worange Point Formation, Se Australia |
title_full |
Palaeomagnetism of Red Beds of the Late Devonian Worange Point Formation, Se Australia |
title_fullStr |
Palaeomagnetism of Red Beds of the Late Devonian Worange Point Formation, Se Australia |
title_full_unstemmed |
Palaeomagnetism of Red Beds of the Late Devonian Worange Point Formation, Se Australia |
title_sort |
palaeomagnetism of red beds of the late devonian worange point formation, se australia |
publishDate |
1991 |
url |
https://researchers.mq.edu.au/en/publications/28367a5f-0ad5-413d-9e8b-43313877d3af https://doi.org/10.1111/j.1365-246X.1991.tb02503.x http://www.scopus.com/inward/record.url?scp=0026053178&partnerID=8YFLogxK |
geographic |
South Pole |
geographic_facet |
South Pole |
genre |
South pole |
genre_facet |
South pole |
op_source |
Thrupp , G A , Kent , D V , Schmidt , P W & Powell , C M 1991 , ' Palaeomagnetism of Red Beds of the Late Devonian Worange Point Formation, Se Australia ' , Geophysical Journal International , vol. 104 , no. 1 , pp. 179-202 . https://doi.org/10.1111/j.1365-246X.1991.tb02503.x |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1111/j.1365-246X.1991.tb02503.x |
container_title |
Geophysical Journal International |
container_volume |
104 |
container_issue |
1 |
container_start_page |
179 |
op_container_end_page |
202 |
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1766202817275494400 |