Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Bindi L. [4]"'
Publikováno v:
Lithos (Oslo. Print) 366-367 (2020): 1–14. doi:10.1016/j.lithos.2020.105539
info:cnr-pdr/source/autori:Matrosova E.A.[1], Bobrov A.V.[1,2,3], Bindi L.[4,5], Pushcharovsky D.Y.[2], Irifune T.[6,7]/titolo:Titanium-rich phases in the Earth's transition zone and lower mantle: Evidence from experiments in the system MgO-SiO2-TiO2(±Al2O3) at 10-24 GPa and 1600 °C/doi:10.1016%2Fj.lithos.2020.105539/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:1/pagina_a:14/intervallo_pagine:1–14/volume:366-367
info:cnr-pdr/source/autori:Matrosova E.A.[1], Bobrov A.V.[1,2,3], Bindi L.[4,5], Pushcharovsky D.Y.[2], Irifune T.[6,7]/titolo:Titanium-rich phases in the Earth's transition zone and lower mantle: Evidence from experiments in the system MgO-SiO2-TiO2(±Al2O3) at 10-24 GPa and 1600 °C/doi:10.1016%2Fj.lithos.2020.105539/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:1/pagina_a:14/intervallo_pagine:1–14/volume:366-367
Phase relations in the MgSiO3-MgTiO3 and Mg3Al2Si3O12-MgTiO3 systems were studied at 10-24 GPa and 1600 °C using a high-pressure Kawai-type multianvil apparatus. We investigated the full range of starting compositions for the enstatite-geikielite sy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::af3a2b3630bb2be484ad4f7c614a1bdc
https://doi.org/10.1016/j.lithos.2020.105539
https://doi.org/10.1016/j.lithos.2020.105539
Publikováno v:
European journal of mineralogy
26 (2014): 427–437. doi:10.1127/0935-1221/2014/0026-2382
info:cnr-pdr/source/autori:Biagioni C.[1], Orlandi P. [1,2], Pasero M.[1], Nestola F.[3], Bindi L. [4]/titolo:Mapiquiroite, (Sr,Pb)(U,Y)Fe2(Ti,Fe3+) 18O38, a new member of the crichtonite group from the Apuan Alps, Tuscany, Italy/doi:10.1127%2F0935-1221%2F2014%2F0026-2382/rivista:European journal of mineralogy (Print)/anno:2014/pagina_da:427/pagina_a:437/intervallo_pagine:427–437/volume:26
26 (2014): 427–437. doi:10.1127/0935-1221/2014/0026-2382
info:cnr-pdr/source/autori:Biagioni C.[1], Orlandi P. [1,2], Pasero M.[1], Nestola F.[3], Bindi L. [4]/titolo:Mapiquiroite, (Sr,Pb)(U,Y)Fe2(Ti,Fe3+) 18O38, a new member of the crichtonite group from the Apuan Alps, Tuscany, Italy/doi:10.1127%2F0935-1221%2F2014%2F0026-2382/rivista:European journal of mineralogy (Print)/anno:2014/pagina_da:427/pagina_a:437/intervallo_pagine:427–437/volume:26
Mapiquiroite, (Sr,Pb)(U,Y)Fe 2 (Ti,Fe 3+ ) 18 O 38 , was identified as a new mineral from the baryte + pyrite + iron oxide ores of Buca della Vena (BdV) and Monte Arsiccio (MA) mines, Apuan Alps, Tuscany, Italy. At BdV, mapiquiroite occurs as complex
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3cf02d4a3464f4ece7513883e9c8dce3
http://hdl.handle.net/11568/491078
http://hdl.handle.net/11568/491078
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