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Thermoelasticity, cation exchange, and deprotonation in Fe-rich holmquistite: Toward a crystal-chemical model for the high-temperature behavior of orthorhombic amphiboles

Autor: Oberti R.[1], Boiocchi M.[2], Zema M.[1

Publikováno v: The American mineralogist 104 (2019): 1829–1839. doi:10.2138/am-2019-6966
info:cnr-pdr/source/autori:Oberti R.[1], Boiocchi M.[2], Zema M.[1,3]/titolo:Thermoelasticity, cation exchange, and deprotonation in Fe-rich holmquistite: Toward a crystal-chemical model for the high-temperature behavior of orthorhombic amphiboles/doi:10.2138%2Fam-2019-6966/rivista:The American mineralogist/anno:2019/pagina_da:1829/pagina_a:1839/intervallo_pagine:1829–1839/volume:104

The thermoelastic behavior of a crystal of Fe-rich holmquistite with crystal-chemical formula A(K0.01Na0.01)B(Li1.88Mg0.10Na0.02)C(Mg1.68Fe1.422+Mn0.022+Al1.88)TSi8.00O22W[(OH)1.97F0.03] was studied by single-crystal X-ray diffraction at temperatures

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3eaa8895c4286c31b31ee7d0de11410a
https://doi.org/10.2138/am-2019-6966

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

Autor: Mihailova B.[1], Della Ventura G.[2, Waeselmann N.[1], Xu W.[4], Schlüter J.[5], Galdenzi F.[2, Marcelli A.[3, Redhammer G.J.[7], Boiocchi M.[8], Oberti R.[9]

Publikováno v: Communications materials 2 (2021): 1–10. doi:10.1038/s43246-021-00161-y
info:cnr-pdr/source/autori:Mihailova B.[1], Della Ventura G.[2,3], Waeselmann N.[1], Xu W.[4], Schlüter J.[5], Galdenzi F.[2,3], Marcelli A.[3,6], Redhammer G.J.[7], Boiocchi M.[8], Oberti R.[9]/titolo:Atomistic insight into lithospheric conductivity revealed by phonon-electron excitations in hydrous iron-bearing silicates/doi:10.1038%2Fs43246-021-00161-y/rivista:Communications materials/anno:2021/pagina_da:1/pagina_a:10/intervallo_pagine:1–10/volume:2
Communications Materials, Vol 2, Iss 1, Pp 1-10 (2021)

Amphiboles are essential components of the continental crust and subduction zones showing anomalous anisotropic conductivity. Rock properties depend on the physical properties of their constituent minerals, which in turn depend on the crystal phonon

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::89f52faed313de873f1c4341da3f2eda
https://hdl.handle.net/11590/424697

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Akademický článek

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The crystal structure of beryllonite from the type locality and comparison with isopointal structures

Autor: Callegari A.M.[1], Boiocchi M.[2], Zema M.[1, Tarantino S.C.[3

Publikováno v: Neues Jahrbuch für Mineralogie. Abhandlungen 197 (2021): 107–119. doi:10.1127/njma/2021/0259
info:cnr-pdr/source/autori:Callegari A.M.[1], Boiocchi M.[2], Zema M.[1,3], Tarantino S.C.[3,4]/titolo:The crystal structure of beryllonite from the type locality and comparison with isopointal structures/doi:10.1127%2Fnjma%2F2021%2F0259/rivista:Neues Jahrbuch für Mineralogie. Abhandlungen/anno:2021/pagina_da:107/pagina_a:119/intervallo_pagine:107–119/volume:197

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Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::638ab34cd3e1679869c5b00b9d9be1ea
https://www.schweizerbart.de/journals/njma

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