Uplift of the central transantarctic mountains

The source of the Transantarctic Mountains’ high elevation has remained unclear. Here, the authors present data from a 550 km long magnetotelluric geophysical transect showing that uplift is likely to be mechanical via cantilevered flexure along a master boundary fault and not upper mantle or lower...

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Autores principales:	Phil Wannamaker, Graham Hill, John Stodt, Virginie Maris, Yasuo Ogawa, Kate Selway, Goran Boren, Edward Bertrand, Daniel Uhlmann, Bridget Ayling, A. Marie Green, Daniel Feucht
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2017
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/a8af31a903104e0ea8fceb4b0201a316
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spelling	oai:doaj.org-article:a8af31a903104e0ea8fceb4b0201a3162021-12-02T14:41:20ZUplift of the central transantarctic mountains10.1038/s41467-017-01577-22041-1723https://doaj.org/article/a8af31a903104e0ea8fceb4b0201a3162017-11-01T00:00:00Zhttps://doi.org/10.1038/s41467-017-01577-2https://doaj.org/toc/2041-1723The source of the Transantarctic Mountains’ high elevation has remained unclear. Here, the authors present data from a 550 km long magnetotelluric geophysical transect showing that uplift is likely to be mechanical via cantilevered flexure along a master boundary fault and not upper mantle or lower crustal thermal mechanisms.Phil WannamakerGraham HillJohn StodtVirginie MarisYasuo OgawaKate SelwayGoran BorenEdward BertrandDaniel UhlmannBridget AylingA. Marie GreenDaniel FeuchtNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-11 (2017)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Phil Wannamaker Graham Hill John Stodt Virginie Maris Yasuo Ogawa Kate Selway Goran Boren Edward Bertrand Daniel Uhlmann Bridget Ayling A. Marie Green Daniel Feucht Uplift of the central transantarctic mountains
description	The source of the Transantarctic Mountains’ high elevation has remained unclear. Here, the authors present data from a 550 km long magnetotelluric geophysical transect showing that uplift is likely to be mechanical via cantilevered flexure along a master boundary fault and not upper mantle or lower crustal thermal mechanisms.
format	article
author	Phil Wannamaker Graham Hill John Stodt Virginie Maris Yasuo Ogawa Kate Selway Goran Boren Edward Bertrand Daniel Uhlmann Bridget Ayling A. Marie Green Daniel Feucht
author_facet	Phil Wannamaker Graham Hill John Stodt Virginie Maris Yasuo Ogawa Kate Selway Goran Boren Edward Bertrand Daniel Uhlmann Bridget Ayling A. Marie Green Daniel Feucht
author_sort	Phil Wannamaker
title	Uplift of the central transantarctic mountains
title_short	Uplift of the central transantarctic mountains
title_full	Uplift of the central transantarctic mountains
title_fullStr	Uplift of the central transantarctic mountains
title_full_unstemmed	Uplift of the central transantarctic mountains
title_sort	uplift of the central transantarctic mountains
publisher	Nature Portfolio
publishDate	2017
url	https://doaj.org/article/a8af31a903104e0ea8fceb4b0201a316
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Uplift of the central transantarctic mountains

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