Atomistic insight into lithospheric conductivity revealed by phonon–electron excitations in hydrous iron-bearing silicates

Amphiboles are hydrous silicates occurring in many rock types in the continental crust and subduction zones. Here, in situ Raman spectroscopy of grunerite reveals temperature-activated electron-phonon excitations that provide an atomistic insight into the role of amphiboles in the anisotropic lithos...

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Autores principales:	Boriana Mihailova, Giancarlo Della Ventura, Naemi Waeselmann, Wei Xu, Jochen Schlüter, Federico Galdenzi, Augusto Marcelli, Günther J. Redhammer, Massimo Boiocchi, Roberta Oberti
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Materials of engineering and construction. Mechanics of materials TA401-492
Acceso en línea:	https://doaj.org/article/b77bc27b819c4cf6b932d96de4f4dd46
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spelling	oai:doaj.org-article:b77bc27b819c4cf6b932d96de4f4dd462021-12-02T15:56:55ZAtomistic insight into lithospheric conductivity revealed by phonon–electron excitations in hydrous iron-bearing silicates10.1038/s43246-021-00161-y2662-4443https://doaj.org/article/b77bc27b819c4cf6b932d96de4f4dd462021-06-01T00:00:00Zhttps://doi.org/10.1038/s43246-021-00161-yhttps://doaj.org/toc/2662-4443Amphiboles are hydrous silicates occurring in many rock types in the continental crust and subduction zones. Here, in situ Raman spectroscopy of grunerite reveals temperature-activated electron-phonon excitations that provide an atomistic insight into the role of amphiboles in the anisotropic lithospheric conductivity.Boriana MihailovaGiancarlo Della VenturaNaemi WaeselmannWei XuJochen SchlüterFederico GaldenziAugusto MarcelliGünther J. RedhammerMassimo BoiocchiRoberta ObertiNature PortfolioarticleMaterials of engineering and construction. Mechanics of materialsTA401-492ENCommunications Materials, Vol 2, Iss 1, Pp 1-10 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Materials of engineering and construction. Mechanics of materials TA401-492
spellingShingle	Materials of engineering and construction. Mechanics of materials TA401-492 Boriana Mihailova Giancarlo Della Ventura Naemi Waeselmann Wei Xu Jochen Schlüter Federico Galdenzi Augusto Marcelli Günther J. Redhammer Massimo Boiocchi Roberta Oberti Atomistic insight into lithospheric conductivity revealed by phonon–electron excitations in hydrous iron-bearing silicates
description	Amphiboles are hydrous silicates occurring in many rock types in the continental crust and subduction zones. Here, in situ Raman spectroscopy of grunerite reveals temperature-activated electron-phonon excitations that provide an atomistic insight into the role of amphiboles in the anisotropic lithospheric conductivity.
format	article
author	Boriana Mihailova Giancarlo Della Ventura Naemi Waeselmann Wei Xu Jochen Schlüter Federico Galdenzi Augusto Marcelli Günther J. Redhammer Massimo Boiocchi Roberta Oberti
author_facet	Boriana Mihailova Giancarlo Della Ventura Naemi Waeselmann Wei Xu Jochen Schlüter Federico Galdenzi Augusto Marcelli Günther J. Redhammer Massimo Boiocchi Roberta Oberti
author_sort	Boriana Mihailova
title	Atomistic insight into lithospheric conductivity revealed by phonon–electron excitations in hydrous iron-bearing silicates
title_short	Atomistic insight into lithospheric conductivity revealed by phonon–electron excitations in hydrous iron-bearing silicates
title_full	Atomistic insight into lithospheric conductivity revealed by phonon–electron excitations in hydrous iron-bearing silicates
title_fullStr	Atomistic insight into lithospheric conductivity revealed by phonon–electron excitations in hydrous iron-bearing silicates
title_full_unstemmed	Atomistic insight into lithospheric conductivity revealed by phonon–electron excitations in hydrous iron-bearing silicates
title_sort	atomistic insight into lithospheric conductivity revealed by phonon–electron excitations in hydrous iron-bearing silicates
publisher	Nature Portfolio
publishDate	2021
url	https://doaj.org/article/b77bc27b819c4cf6b932d96de4f4dd46
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Atomistic insight into lithospheric conductivity revealed by phonon–electron excitations in hydrous iron-bearing silicates

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