A multi-domain lithospheric model of East Antarctica
The geology of East Antarctica is poorly constrained and covered by ice which can be several kilometers thick,however, these hidden and inaccessible rocks are of major interest in interdisciplinary studies linking the solidEarth and cryosphere. Subglacial geothermal heat flux is an important paramet...
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ftunivtasecite:oai:ecite.utas.edu.au:131207 2023-05-15T13:55:18+02:00 A multi-domain lithospheric model of East Antarctica Staal, T Reading, AM Halpin, J Whittaker, J 2018 application/pdf https://www.polar2018.org/ http://ecite.utas.edu.au/131207 en eng . http://ecite.utas.edu.au/131207/1/polar2018_abstractproceedings 1938.pdf Staal, T and Reading, AM and Halpin, J and Whittaker, J, A multi-domain lithospheric model of East Antarctica, POLAR2018 Open Science Conference Abstract Proceedings, 19-23 June 2018, Davos, Switzerland, pp. 1938. (2018) [Conference Extract] http://ecite.utas.edu.au/131207 Mathematical Sciences Statistics Probability Theory Conference Extract NonPeerReviewed 2018 ftunivtasecite 2019-12-13T22:29:08Z The geology of East Antarctica is poorly constrained and covered by ice which can be several kilometers thick,however, these hidden and inaccessible rocks are of major interest in interdisciplinary studies linking the solidEarth and cryosphere. Subglacial geothermal heat flux is an important parameter for ice sheet models anddepends on heat production within the crust, but also the deep geothermal gradient that is defined by thelithospheric structure. Seismic tomography studies derive lithosphere thickness and structure, but the resolution is relatively low, andthe smoothed models don't reflect the amalgamation of lithospheric terranes that formed the continent. Wecombine geophysical constraints from seismic properties and potential field data, with geological knowledgefrom the sparse Antarctic outcrops and from Gondwanan neighbours in a plate reconstruction framework. Weuse Bayesian inference to suggest the most probable boundaries by using a multivariate prior. The boundariesform a segmentation of the Antarctic lithosphere and can be weighted with probabilistic significance andlocation. The result is presented as a first draft of a multi-domain tessellated terrane map of the East Antarcticlithosphere. We believe that this approach will be useful in estimating both basal lithosphere and crustalcontributions to heat flux, and is a robust stepping stone towards more refined models. Conference Object Antarc* Antarctic Antarctica East Antarctica Ice Sheet eCite UTAS (University of Tasmania) Antarctic The Antarctic East Antarctica |
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Open Polar |
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eCite UTAS (University of Tasmania) |
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ftunivtasecite |
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English |
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Mathematical Sciences Statistics Probability Theory |
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Mathematical Sciences Statistics Probability Theory Staal, T Reading, AM Halpin, J Whittaker, J A multi-domain lithospheric model of East Antarctica |
topic_facet |
Mathematical Sciences Statistics Probability Theory |
description |
The geology of East Antarctica is poorly constrained and covered by ice which can be several kilometers thick,however, these hidden and inaccessible rocks are of major interest in interdisciplinary studies linking the solidEarth and cryosphere. Subglacial geothermal heat flux is an important parameter for ice sheet models anddepends on heat production within the crust, but also the deep geothermal gradient that is defined by thelithospheric structure. Seismic tomography studies derive lithosphere thickness and structure, but the resolution is relatively low, andthe smoothed models don't reflect the amalgamation of lithospheric terranes that formed the continent. Wecombine geophysical constraints from seismic properties and potential field data, with geological knowledgefrom the sparse Antarctic outcrops and from Gondwanan neighbours in a plate reconstruction framework. Weuse Bayesian inference to suggest the most probable boundaries by using a multivariate prior. The boundariesform a segmentation of the Antarctic lithosphere and can be weighted with probabilistic significance andlocation. The result is presented as a first draft of a multi-domain tessellated terrane map of the East Antarcticlithosphere. We believe that this approach will be useful in estimating both basal lithosphere and crustalcontributions to heat flux, and is a robust stepping stone towards more refined models. |
format |
Conference Object |
author |
Staal, T Reading, AM Halpin, J Whittaker, J |
author_facet |
Staal, T Reading, AM Halpin, J Whittaker, J |
author_sort |
Staal, T |
title |
A multi-domain lithospheric model of East Antarctica |
title_short |
A multi-domain lithospheric model of East Antarctica |
title_full |
A multi-domain lithospheric model of East Antarctica |
title_fullStr |
A multi-domain lithospheric model of East Antarctica |
title_full_unstemmed |
A multi-domain lithospheric model of East Antarctica |
title_sort |
multi-domain lithospheric model of east antarctica |
publisher |
. |
publishDate |
2018 |
url |
https://www.polar2018.org/ http://ecite.utas.edu.au/131207 |
geographic |
Antarctic The Antarctic East Antarctica |
geographic_facet |
Antarctic The Antarctic East Antarctica |
genre |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet |
op_relation |
http://ecite.utas.edu.au/131207/1/polar2018_abstractproceedings 1938.pdf Staal, T and Reading, AM and Halpin, J and Whittaker, J, A multi-domain lithospheric model of East Antarctica, POLAR2018 Open Science Conference Abstract Proceedings, 19-23 June 2018, Davos, Switzerland, pp. 1938. (2018) [Conference Extract] http://ecite.utas.edu.au/131207 |
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