Metamorphic pressure variation in a coherent Alpine nappe challenges lithostatic pressure paradigm

The geodynamic evolution of mountain ranges can be reconstructed using the pressure recorded by minerals in metamorphic rocks, under the key assumption that rock pressure is lithostatic. Here, the authors challenge the lithostatic pressure paradigm by showing that there can be significant outcrop-sc...

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Auteurs principaux:	Cindy Luisier, Lukas Baumgartner, Stefan M. Schmalholz, Guillaume Siron, Torsten Vennemann
Format:	article
Langue:	EN
Publié:	Nature Portfolio 2019
Sujets:	Science Q
Accès en ligne:	https://doaj.org/article/6583d0c6e5424493aae8e16b2d02a2ff
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id	oai:doaj.org-article:6583d0c6e5424493aae8e16b2d02a2ff
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spelling	oai:doaj.org-article:6583d0c6e5424493aae8e16b2d02a2ff2021-12-02T16:58:27ZMetamorphic pressure variation in a coherent Alpine nappe challenges lithostatic pressure paradigm10.1038/s41467-019-12727-z2041-1723https://doaj.org/article/6583d0c6e5424493aae8e16b2d02a2ff2019-10-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-12727-zhttps://doaj.org/toc/2041-1723The geodynamic evolution of mountain ranges can be reconstructed using the pressure recorded by minerals in metamorphic rocks, under the key assumption that rock pressure is lithostatic. Here, the authors challenge the lithostatic pressure paradigm by showing that there can be significant outcrop-scale pressure gradients due to compression- and reaction-induced stress.Cindy LuisierLukas BaumgartnerStefan M. SchmalholzGuillaume SironTorsten VennemannNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-11 (2019)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Cindy Luisier Lukas Baumgartner Stefan M. Schmalholz Guillaume Siron Torsten Vennemann Metamorphic pressure variation in a coherent Alpine nappe challenges lithostatic pressure paradigm
description	The geodynamic evolution of mountain ranges can be reconstructed using the pressure recorded by minerals in metamorphic rocks, under the key assumption that rock pressure is lithostatic. Here, the authors challenge the lithostatic pressure paradigm by showing that there can be significant outcrop-scale pressure gradients due to compression- and reaction-induced stress.
format	article
author	Cindy Luisier Lukas Baumgartner Stefan M. Schmalholz Guillaume Siron Torsten Vennemann
author_facet	Cindy Luisier Lukas Baumgartner Stefan M. Schmalholz Guillaume Siron Torsten Vennemann
author_sort	Cindy Luisier
title	Metamorphic pressure variation in a coherent Alpine nappe challenges lithostatic pressure paradigm
title_short	Metamorphic pressure variation in a coherent Alpine nappe challenges lithostatic pressure paradigm
title_full	Metamorphic pressure variation in a coherent Alpine nappe challenges lithostatic pressure paradigm
title_fullStr	Metamorphic pressure variation in a coherent Alpine nappe challenges lithostatic pressure paradigm
title_full_unstemmed	Metamorphic pressure variation in a coherent Alpine nappe challenges lithostatic pressure paradigm
title_sort	metamorphic pressure variation in a coherent alpine nappe challenges lithostatic pressure paradigm
publisher	Nature Portfolio
publishDate	2019
url	https://doaj.org/article/6583d0c6e5424493aae8e16b2d02a2ff
work_keys_str_mv	AT cindyluisier metamorphicpressurevariationinacoherentalpinenappechallengeslithostaticpressureparadigm AT lukasbaumgartner metamorphicpressurevariationinacoherentalpinenappechallengeslithostaticpressureparadigm AT stefanmschmalholz metamorphicpressurevariationinacoherentalpinenappechallengeslithostaticpressureparadigm AT guillaumesiron metamorphicpressurevariationinacoherentalpinenappechallengeslithostaticpressureparadigm AT torstenvennemann metamorphicpressurevariationinacoherentalpinenappechallengeslithostaticpressureparadigm
_version_	1718382331143651328

Metamorphic pressure variation in a coherent Alpine nappe challenges lithostatic pressure paradigm

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