The present configuration of the Bouvet triple junction
New Hawaii-MRI sonar data show that the southernmost Mid-Atlantic Ridge joins the South American-Antarctic Ridge by an obliquely opening rift and overlaps Spiess Ridge, the westernmost segment of the Southwest Indian Ridge, with no evidence for a transform fault. The junction is therefore neither ri...
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ftumanchesterpub:oai:pure.atira.dk:publications/0cbedbd1-d065-4bf6-aa40-e9b5b20ae219 2023-11-12T04:08:29+01:00 The present configuration of the Bouvet triple junction Mitchell, N. C. Livermore, R. A. 1998 https://research.manchester.ac.uk/en/publications/0cbedbd1-d065-4bf6-aa40-e9b5b20ae219 https://doi.org/10.1130/0091-7613(1998)026<0267:TPCOTB>2.3.CO;2 http://://000072436000019 eng eng info:eu-repo/semantics/closedAccess Mitchell , N C & Livermore , R A 1998 , ' The present configuration of the Bouvet triple junction ' , Geology , vol. 26 , no. 3 , pp. 267-270 . https://doi.org/10.1130/0091-7613(1998)026<0267:TPCOTB>2.3.CO;2 article 1998 ftumanchesterpub https://doi.org/10.1130/0091-7613(1998)026<0267:TPCOTB>2.3.CO;2 2023-10-30T09:17:14Z New Hawaii-MRI sonar data show that the southernmost Mid-Atlantic Ridge joins the South American-Antarctic Ridge by an obliquely opening rift and overlaps Spiess Ridge, the westernmost segment of the Southwest Indian Ridge, with no evidence for a transform fault. The junction is therefore neither ridge-fault-fault nor ridge-ridge-ridge. We speculate that growth of Spiess Ridge adjacent to the triple junction has caused this complexity and discuss more generally the origins of distributed deformation of oceanic triple junctions. Article in Journal/Newspaper Antarc* Antarctic The University of Manchester: Research Explorer Antarctic Indian Mid-Atlantic Ridge Bouvet ENVELOPE(3.358,3.358,-54.422,-54.422) |
institution |
Open Polar |
collection |
The University of Manchester: Research Explorer |
op_collection_id |
ftumanchesterpub |
language |
English |
description |
New Hawaii-MRI sonar data show that the southernmost Mid-Atlantic Ridge joins the South American-Antarctic Ridge by an obliquely opening rift and overlaps Spiess Ridge, the westernmost segment of the Southwest Indian Ridge, with no evidence for a transform fault. The junction is therefore neither ridge-fault-fault nor ridge-ridge-ridge. We speculate that growth of Spiess Ridge adjacent to the triple junction has caused this complexity and discuss more generally the origins of distributed deformation of oceanic triple junctions. |
format |
Article in Journal/Newspaper |
author |
Mitchell, N. C. Livermore, R. A. |
spellingShingle |
Mitchell, N. C. Livermore, R. A. The present configuration of the Bouvet triple junction |
author_facet |
Mitchell, N. C. Livermore, R. A. |
author_sort |
Mitchell, N. C. |
title |
The present configuration of the Bouvet triple junction |
title_short |
The present configuration of the Bouvet triple junction |
title_full |
The present configuration of the Bouvet triple junction |
title_fullStr |
The present configuration of the Bouvet triple junction |
title_full_unstemmed |
The present configuration of the Bouvet triple junction |
title_sort |
present configuration of the bouvet triple junction |
publishDate |
1998 |
url |
https://research.manchester.ac.uk/en/publications/0cbedbd1-d065-4bf6-aa40-e9b5b20ae219 https://doi.org/10.1130/0091-7613(1998)026<0267:TPCOTB>2.3.CO;2 http://://000072436000019 |
long_lat |
ENVELOPE(3.358,3.358,-54.422,-54.422) |
geographic |
Antarctic Indian Mid-Atlantic Ridge Bouvet |
geographic_facet |
Antarctic Indian Mid-Atlantic Ridge Bouvet |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
Mitchell , N C & Livermore , R A 1998 , ' The present configuration of the Bouvet triple junction ' , Geology , vol. 26 , no. 3 , pp. 267-270 . https://doi.org/10.1130/0091-7613(1998)026<0267:TPCOTB>2.3.CO;2 |
op_rights |
info:eu-repo/semantics/closedAccess |
op_doi |
https://doi.org/10.1130/0091-7613(1998)026<0267:TPCOTB>2.3.CO;2 |
_version_ |
1782328768462848000 |