Extension along the Australian-Pacific transpressional transform plate boundary near Macquarie Island
The Australian-Pacific transform plate boundary fault zone along the Macquarie and McDougallsegments of the Macquarie Ridge Complex (MRC), south of New Zealand, is characterized by dominantlynormal faults and pull-apart basins, in apparent conflict with the regional transpressional tectonic setting....
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Online Access: | https://doi.org/10.1029/2003GC000523 http://ecite.utas.edu.au/73794 |
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ftunivtasecite:oai:ecite.utas.edu.au:73794 2023-05-15T17:09:52+02:00 Extension along the Australian-Pacific transpressional transform plate boundary near Macquarie Island Daczko, NR Wertz, KL Mosher, S Coffin, MF Meckel, TA 2003 application/pdf https://doi.org/10.1029/2003GC000523 http://ecite.utas.edu.au/73794 en eng Amer Geophysical Union http://ecite.utas.edu.au/73794/1/Daczko_et_al_G3_2003.pdf http://dx.doi.org/10.1029/2003GC000523 Daczko, NR and Wertz, KL and Mosher, S and Coffin, MF and Meckel, TA, Extension along the Australian-Pacific transpressional transform plate boundary near Macquarie Island, Geochemistry Geophysics Geosystems, 4, (9) EJ ISSN 1525-2027 (2003) [Refereed Article] http://ecite.utas.edu.au/73794 Earth Sciences Geology Marine geoscience Refereed Article PeerReviewed 2003 ftunivtasecite https://doi.org/10.1029/2003GC000523 2022-08-29T22:16:42Z The Australian-Pacific transform plate boundary fault zone along the Macquarie and McDougallsegments of the Macquarie Ridge Complex (MRC), south of New Zealand, is characterized by dominantlynormal faults and pull-apart basins, in apparent conflict with the regional transpressional tectonic setting.We propose that present-day curvature of the transform is inherited from a preexisting divergent plateboundary and that the overall extensional kinematics shown by faults along the main plate boundary traceand exposed on Macquarie Island result from local stresses related to right-lateral, right stepping, enechelon plate boundary faults and not to the current transpressional setting. Transpression along theAustralian-Pacific transform plate boundary has resulted in uplift along the ~1500 km long MacquarieRidge Complex. Macquarie Island, the only subaerial exposure of the complex, sits atop a ~5 km high,~50 km wide submarine ridge of oceanic crust and lies ~4.5 km east of the major active plate boundaryfault zone. Thus Macquarie Island and the surrounding seafloor provide a unique opportunity to study anactive oceanic transform fault using complementary marine geophysical and land-based geological data.Mapping of recent faults affecting the topography of Macquarie Island shows that the island is extensivelycut by high-angle normal faults forming pull-apart basins. Furthermore, evidence for reverse motion israre. Using marine geophysical data, including swath bathymetry, reflectivity, and seismic reflection data,collected along the Australian-Pacific plate boundary north and south of the island, we have defined a 5-15 km wide plate boundary zone. A series of right stepping en echelon faults, within this zone, liesalong the main plate boundary trace. At the right stepping fault terminations, elongate depressions (<=10 kmwide and 1.2 km deep) parallel the plate boundary, which we interpret as extensional relay zones or pullapartbasins. We propose that transpression is partitioned into en echelon strike-slip faults at ... Article in Journal/Newspaper Macquarie Island eCite UTAS (University of Tasmania) New Zealand Pacific Geochemistry, Geophysics, Geosystems 4 9 n/a n/a |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Geology Marine geoscience |
spellingShingle |
Earth Sciences Geology Marine geoscience Daczko, NR Wertz, KL Mosher, S Coffin, MF Meckel, TA Extension along the Australian-Pacific transpressional transform plate boundary near Macquarie Island |
topic_facet |
Earth Sciences Geology Marine geoscience |
description |
The Australian-Pacific transform plate boundary fault zone along the Macquarie and McDougallsegments of the Macquarie Ridge Complex (MRC), south of New Zealand, is characterized by dominantlynormal faults and pull-apart basins, in apparent conflict with the regional transpressional tectonic setting.We propose that present-day curvature of the transform is inherited from a preexisting divergent plateboundary and that the overall extensional kinematics shown by faults along the main plate boundary traceand exposed on Macquarie Island result from local stresses related to right-lateral, right stepping, enechelon plate boundary faults and not to the current transpressional setting. Transpression along theAustralian-Pacific transform plate boundary has resulted in uplift along the ~1500 km long MacquarieRidge Complex. Macquarie Island, the only subaerial exposure of the complex, sits atop a ~5 km high,~50 km wide submarine ridge of oceanic crust and lies ~4.5 km east of the major active plate boundaryfault zone. Thus Macquarie Island and the surrounding seafloor provide a unique opportunity to study anactive oceanic transform fault using complementary marine geophysical and land-based geological data.Mapping of recent faults affecting the topography of Macquarie Island shows that the island is extensivelycut by high-angle normal faults forming pull-apart basins. Furthermore, evidence for reverse motion israre. Using marine geophysical data, including swath bathymetry, reflectivity, and seismic reflection data,collected along the Australian-Pacific plate boundary north and south of the island, we have defined a 5-15 km wide plate boundary zone. A series of right stepping en echelon faults, within this zone, liesalong the main plate boundary trace. At the right stepping fault terminations, elongate depressions (<=10 kmwide and 1.2 km deep) parallel the plate boundary, which we interpret as extensional relay zones or pullapartbasins. We propose that transpression is partitioned into en echelon strike-slip faults at ... |
format |
Article in Journal/Newspaper |
author |
Daczko, NR Wertz, KL Mosher, S Coffin, MF Meckel, TA |
author_facet |
Daczko, NR Wertz, KL Mosher, S Coffin, MF Meckel, TA |
author_sort |
Daczko, NR |
title |
Extension along the Australian-Pacific transpressional transform plate boundary near Macquarie Island |
title_short |
Extension along the Australian-Pacific transpressional transform plate boundary near Macquarie Island |
title_full |
Extension along the Australian-Pacific transpressional transform plate boundary near Macquarie Island |
title_fullStr |
Extension along the Australian-Pacific transpressional transform plate boundary near Macquarie Island |
title_full_unstemmed |
Extension along the Australian-Pacific transpressional transform plate boundary near Macquarie Island |
title_sort |
extension along the australian-pacific transpressional transform plate boundary near macquarie island |
publisher |
Amer Geophysical Union |
publishDate |
2003 |
url |
https://doi.org/10.1029/2003GC000523 http://ecite.utas.edu.au/73794 |
geographic |
New Zealand Pacific |
geographic_facet |
New Zealand Pacific |
genre |
Macquarie Island |
genre_facet |
Macquarie Island |
op_relation |
http://ecite.utas.edu.au/73794/1/Daczko_et_al_G3_2003.pdf http://dx.doi.org/10.1029/2003GC000523 Daczko, NR and Wertz, KL and Mosher, S and Coffin, MF and Meckel, TA, Extension along the Australian-Pacific transpressional transform plate boundary near Macquarie Island, Geochemistry Geophysics Geosystems, 4, (9) EJ ISSN 1525-2027 (2003) [Refereed Article] http://ecite.utas.edu.au/73794 |
op_doi |
https://doi.org/10.1029/2003GC000523 |
container_title |
Geochemistry, Geophysics, Geosystems |
container_volume |
4 |
container_issue |
9 |
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1766066232335794176 |