Crustal structure of the east Gondwana margin in southeast Australia revealed by transdimensional ambient seismic noise tomography
Ambient seismic noise data from the ongoing WOMBAT transportable seismic array in southeast Australia, the largest deployment of its kind in the Southern Hemisphere, are used to produce a high‐resolution 3‐D shear wave velocity model of the region. We apply a two‐stage, transdimensional, hierarchica...
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Published in: | Geophysical research letters Vol. 40; no. 16; pp. 4266 - 4271 |
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Main Authors: | , , , , , |
Format: | Journal Article |
Language: | English |
Published: |
Washington, DC
Blackwell Publishing Ltd
28-08-2013
American Geophysical Union John Wiley & Sons, Inc |
Subjects: | |
Online Access: | Get full text |
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Summary: | Ambient seismic noise data from the ongoing WOMBAT transportable seismic array in southeast Australia, the largest deployment of its kind in the Southern Hemisphere, are used to produce a high‐resolution 3‐D shear wave velocity model of the region. We apply a two‐stage, transdimensional, hierarchical Bayesian inversion approach to recover phase velocity maps at periods of 1–20 s and then invert phase velocity dispersion for 3‐D shear wave velocity structure to the base of the crust. Data uncertainty is propagated through the sequence of inversions, ensuring that model complexity is justified by the quality and quantity of the measurements. The pattern of 3‐D velocity variations helps elucidate the geometry and position of key crustal features—such as the Torrens Hinge Zone—associated with the transition from Paleozoic eastern Australia to Precambrian central and western Australia that formed along the proto‐Pacific margin of east Gondwana.
Key Points
Large ambient noise dataset reveals new insight into east Gondwana margin
Bayesian transdimensional tomography achieves superior results
Candidate for the Tasman Line separating east and west Australia revealed |
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Bibliography: | ArticleID:GRL50878 Supporting informationSupporting informationSupporting informationSupporting informationSupporting informationSupporting informationSupporting informationSupporting informationSupporting informationSupporting information istex:F4EBEC63D9B00EDFCF7F988D4700D65BFE3F6FCD ark:/67375/WNG-6GXM4VR3-T ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0094-8276 1944-8007 |
DOI: | 10.1002/grl.50878 |