Simultaneous rupture along two conjugate planes of the Wharton Basin earthquake.

Analysis of broadband teleseismic data shows that the 18 June 2000 Wharton Basin earthquake, a moment magnitude 7.8 intraplate event in the region of diffuse deformation separating the Indian and Australian plates, consisted of two subevents that simultaneously ruptured two near-conjugate planes. Th...

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Main Authors: Robinson, D, Henry, C, Das, S, Woodhouse, J
Format: Journal article
Language:English
Published: 2001
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author Robinson, D
Henry, C
Das, S
Woodhouse, J
author_facet Robinson, D
Henry, C
Das, S
Woodhouse, J
author_sort Robinson, D
collection OXFORD
description Analysis of broadband teleseismic data shows that the 18 June 2000 Wharton Basin earthquake, a moment magnitude 7.8 intraplate event in the region of diffuse deformation separating the Indian and Australian plates, consisted of two subevents that simultaneously ruptured two near-conjugate planes. This mode of rupture accommodates shortening by a mechanism different from that previously known elsewhere in the region. The larger subevent occurred on a fossil fracture zone, with a relatively high stress drop of about 20 megapascals, showing that large stresses can accumulate in regions of distributed deformation.
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spelling oxford-uuid:1d0b17d4-7a33-4e27-9f23-e79617bce8e82022-03-26T11:08:40ZSimultaneous rupture along two conjugate planes of the Wharton Basin earthquake.Journal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:1d0b17d4-7a33-4e27-9f23-e79617bce8e8EnglishSymplectic Elements at Oxford2001Robinson, DHenry, CDas, SWoodhouse, JAnalysis of broadband teleseismic data shows that the 18 June 2000 Wharton Basin earthquake, a moment magnitude 7.8 intraplate event in the region of diffuse deformation separating the Indian and Australian plates, consisted of two subevents that simultaneously ruptured two near-conjugate planes. This mode of rupture accommodates shortening by a mechanism different from that previously known elsewhere in the region. The larger subevent occurred on a fossil fracture zone, with a relatively high stress drop of about 20 megapascals, showing that large stresses can accumulate in regions of distributed deformation.
spellingShingle Robinson, D
Henry, C
Das, S
Woodhouse, J
Simultaneous rupture along two conjugate planes of the Wharton Basin earthquake.
title Simultaneous rupture along two conjugate planes of the Wharton Basin earthquake.
title_full Simultaneous rupture along two conjugate planes of the Wharton Basin earthquake.
title_fullStr Simultaneous rupture along two conjugate planes of the Wharton Basin earthquake.
title_full_unstemmed Simultaneous rupture along two conjugate planes of the Wharton Basin earthquake.
title_short Simultaneous rupture along two conjugate planes of the Wharton Basin earthquake.
title_sort simultaneous rupture along two conjugate planes of the wharton basin earthquake
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AT henryc simultaneousrupturealongtwoconjugateplanesofthewhartonbasinearthquake
AT dass simultaneousrupturealongtwoconjugateplanesofthewhartonbasinearthquake
AT woodhousej simultaneousrupturealongtwoconjugateplanesofthewhartonbasinearthquake