An effective elastic thickness map of Australia from wavelet transforms of gravity and topography using Forsyth's method

We have developed a wavelet version of Forsyth's coherence method for estimating the effective elasticthickness (T e) of the lithosphere from gravity and topography. We have previously shown that the 'fan' wavelet is particularly well suited to making localised coherence estimates and...

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Main Authors: Swain, Christopher, Kirby, Jonathan
Format: Journal Article
Published: American Geophysical Union 2006
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/20396
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author Swain, Christopher
Kirby, Jonathan
author_facet Swain, Christopher
Kirby, Jonathan
author_sort Swain, Christopher
building Curtin Institutional Repository
collection Online Access
description We have developed a wavelet version of Forsyth's coherence method for estimating the effective elasticthickness (T e) of the lithosphere from gravity and topography. We have previously shown that the 'fan' wavelet is particularly well suited to making localised coherence estimates and here we progress the method by showing how the coherence can be modelled by using the wavelet transforms of gravity and topography to infer the initial loads that flex the plate. The effectiveness of the method is demonstrated on synthetic data from a model having a rectangular area of large T e embedded in a uniform low T e surrounding, and a load ratio that increases with wave number. The results for the Australia region show a 'core' of high T e under north and central Australia, with much lower values to the east and also, unexpectedly, under the western parts of the Yilgarn and Pilbara cratons.
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institution Curtin University Malaysia
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publishDate 2006
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spelling curtin-20.500.11937-203962019-02-19T04:26:46Z An effective elastic thickness map of Australia from wavelet transforms of gravity and topography using Forsyth's method Swain, Christopher Kirby, Jonathan wavelets Australia coherence Elastic thickness We have developed a wavelet version of Forsyth's coherence method for estimating the effective elasticthickness (T e) of the lithosphere from gravity and topography. We have previously shown that the 'fan' wavelet is particularly well suited to making localised coherence estimates and here we progress the method by showing how the coherence can be modelled by using the wavelet transforms of gravity and topography to infer the initial loads that flex the plate. The effectiveness of the method is demonstrated on synthetic data from a model having a rectangular area of large T e embedded in a uniform low T e surrounding, and a load ratio that increases with wave number. The results for the Australia region show a 'core' of high T e under north and central Australia, with much lower values to the east and also, unexpectedly, under the western parts of the Yilgarn and Pilbara cratons. 2006 Journal Article http://hdl.handle.net/20.500.11937/20396 10.1029/2005GL025090 American Geophysical Union fulltext
spellingShingle wavelets
Australia
coherence
Elastic thickness
Swain, Christopher
Kirby, Jonathan
An effective elastic thickness map of Australia from wavelet transforms of gravity and topography using Forsyth's method
title An effective elastic thickness map of Australia from wavelet transforms of gravity and topography using Forsyth's method
title_full An effective elastic thickness map of Australia from wavelet transforms of gravity and topography using Forsyth's method
title_fullStr An effective elastic thickness map of Australia from wavelet transforms of gravity and topography using Forsyth's method
title_full_unstemmed An effective elastic thickness map of Australia from wavelet transforms of gravity and topography using Forsyth's method
title_short An effective elastic thickness map of Australia from wavelet transforms of gravity and topography using Forsyth's method
title_sort effective elastic thickness map of australia from wavelet transforms of gravity and topography using forsyth's method
topic wavelets
Australia
coherence
Elastic thickness
url http://hdl.handle.net/20.500.11937/20396