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pro vyhledávání: '"Bobrov A. [3]"'
Publikováno v:
The American mineralogist 105 (2021): 132–135. doi:10.2138/am-2020-7204
info:cnr-pdr/source/autori:Bindi L.[1,2], Bendeliani A.[3,4], Bobrov A.[3,4,5], Matrosova E.[4], Irifune T.[6,7]/titolo:Incorporation of Mg in phase Egg, AlSiO3OH: Toward a new polymorph of phase H, MgSiH2O4, a carrier of water in the deep mantle/doi:10.2138%2Fam-2020-7204/rivista:The American mineralogist/anno:2021/pagina_da:132/pagina_a:135/intervallo_pagine:132–135/volume:105
info:cnr-pdr/source/autori:Bindi L.[1,2], Bendeliani A.[3,4], Bobrov A.[3,4,5], Matrosova E.[4], Irifune T.[6,7]/titolo:Incorporation of Mg in phase Egg, AlSiO3OH: Toward a new polymorph of phase H, MgSiH2O4, a carrier of water in the deep mantle/doi:10.2138%2Fam-2020-7204/rivista:The American mineralogist/anno:2021/pagina_da:132/pagina_a:135/intervallo_pagine:132–135/volume:105
The crystal structure and chemical composition of a crystal of Mg-bearing phase Egg with a general formula M1−x3+Mx2+SiO4H1+x (M3+ = Al, Cr; M2+ = Mg, Fe), where x = 0.35, produced by subsolidus reaction at 24 GPa and 1400 °C of components of subd
Autor:
Dymshits A. [1, Bobrov A. [3], Bindi L. [4, Litvin Y. [6], Litasov K. [2, Shatskiy A. [2, Othani E. [7]
Publikováno v:
Geochimica et cosmochimica acta (Online) 105 (2013): 1–13. doi:10.1016/j.gca.2012.11.032
info:cnr-pdr/source/autori:Dymshits A. [1, 2], Bobrov A. [3], Bindi L. [4, 5], Litvin Y. [6], Litasov K. [2, 7], Shatskiy A. [2, 7], Othani E. [7]/titolo:Na-bearing majoritic garnet in the Na2MgSi5O12-Mg3Al2Si3O12 join at 11-20 GPa: Phase relations, structural peculiarities and solid solutions./doi:10.1016%2Fj.gca.2012.11.032/rivista:Geochimica et cosmochimica acta (Online)/anno:2013/pagina_da:1/pagina_a:13/intervallo_pagine:1–13/volume:105
info:cnr-pdr/source/autori:Dymshits A. [1, 2], Bobrov A. [3], Bindi L. [4, 5], Litvin Y. [6], Litasov K. [2, 7], Shatskiy A. [2, 7], Othani E. [7]/titolo:Na-bearing majoritic garnet in the Na2MgSi5O12-Mg3Al2Si3O12 join at 11-20 GPa: Phase relations, structural peculiarities and solid solutions./doi:10.1016%2Fj.gca.2012.11.032/rivista:Geochimica et cosmochimica acta (Online)/anno:2013/pagina_da:1/pagina_a:13/intervallo_pagine:1–13/volume:105
Na-majorite Na 2 MgSi 5 O 12 (NaMaj), an end-member of sodium-rich majoritic garnet, was synthesized and garnet/pyroxene transition was studied in Kawai-type multi-anvil experiments at 11–20 GPa and 1500–2300 °C. Na-majorite was obtained at 16 G
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5f0ee9ab064a2271ae17dfc559bddb9c