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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Main Authors: Mitchell, N. C., Livermore, R. A.
Format: Article in Journal/Newspaper
Language:English
Published: 1998
Subjects:
Online Access: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
id ftumanchesterpub:oai:pure.atira.dk:publications/0cbedbd1-d065-4bf6-aa40-e9b5b20ae219
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spelling 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
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