Zobrazeno 1 - 10
of 104
pro vyhledávání: '"Pier Francesco Zanazzi"'
Publikováno v:
Contributions to Mineralogy and Petrology. 162:275-288
Clinopyroxene phenocrysts from the mafic calc-alkaline lavas of Salina (Aeolian arc, southern Tyrrhenian Sea, Italy) have been analysed to determine the hydrogen content and iron oxidation state of this early crystallized phase. The volcanic activity
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::081c7a3a07db48e0e3541ae624cd0aaf
https://doi.org/10.1007/s00410-010-0594-z
https://doi.org/10.1007/s00410-010-0594-z
Autor:
C. Capalbo, Paola Comodi, T. Boffa Ballaran, Pier Francesco Zanazzi, A. Zanetti, Sabrina Nazzareni
Publikováno v:
The American mineralogist 95 (2010): 1042–1051. doi:10.2138/am.2010.3429
info:cnr-pdr/source/autori:Comodi P.; Boffa Ballaran T.; Zanazzi P.; Capalbo C.; Zanetti A.; Nazzareni S./titolo:The effect of oxo-component on the high-pressure behavior of amphiboles./doi:10.2138%2Fam.2010.3429/rivista:The American mineralogist/anno:2010/pagina_da:1042/pagina_a:1051/intervallo_pagine:1042–1051/volume:95
info:cnr-pdr/source/autori:Comodi P.; Boffa Ballaran T.; Zanazzi P.; Capalbo C.; Zanetti A.; Nazzareni S./titolo:The effect of oxo-component on the high-pressure behavior of amphiboles./doi:10.2138%2Fam.2010.3429/rivista:The American mineralogist/anno:2010/pagina_da:1042/pagina_a:1051/intervallo_pagine:1042–1051/volume:95
The role of the oxo-component on the compressibility of amphibole was studied by means of high-pressure in situ single-crystal X-ray diffraction on two natural kaersutite megacrysts (samples DL5 and FR12) from alkaline basalts. The oxo-component vari
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c7e12e84cb79d68d7d335f7e9a405f55
https://doi.org/10.2138/am.2010.3429
https://doi.org/10.2138/am.2010.3429
Publikováno v:
American Mineralogist. 94:352-358
An in-situ, high-pressure, single-crystal X-ray diffraction study has been carried out at room temperature up to 7.42 GPa on a crystal of ingersonite, ideally Ca 3 Mn 2+ Sb 4 5+ O 14 , from the type material. Ingersonite is isostructural with the syn
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::86548b86f65cf44aa31e11907581f36e
https://doi.org/10.2138/am.2009.3030
https://doi.org/10.2138/am.2009.3030
Autor:
Nicola Rotiroti, Milan Drábek, Pier Francesco Zanazzi, G. Diego Gatta, M. Rieder, R. Klaska, Zdeněk Weiss
Publikováno v:
American Mineralogist. 93:988-995
Crystalline CsAlSiO 4 was synthesized from a stoichiometric mixture of Al 2 O 3 + SiO 2 + Cs 2 O (plus excess water) in Ag-capsules at hydrostatic pressure of 0.1 GPa and temperature of 695 °C. The duration of synthesis was 46 h. The crystal structu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1591d0fe8f69b48f953b71e48445b764
https://doi.org/10.2138/am.2008.2729
https://doi.org/10.2138/am.2008.2729
Publikováno v:
American Mineralogist. 90:1012-1016
Here we report the results of the first three-dimensional refinement of the 10 A phase performed with single-crystal X-ray data. The 10 A phase, Mg3Si4O10(OH)2H2O, is monoclinic, space group C 2/ m , a = 5.323(1)A, b = 9.203(1)A, c = 10.216(1)A, β =
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1882f10e1121ed2c9a575ad64c47e871
https://doi.org/10.2138/am.2005.1831
https://doi.org/10.2138/am.2005.1831
Publikováno v:
American Mineralogist. 90:645-652
Elastic behavior and high-pressure (HP) structural evolution of a natural zeolite levyne, (Ca 0.5 ,Na,K) 6 (Al 6 Si 12 O 36 )·18H 2 O, has been investigated up to 5 GPa by means of in situ single-crystal X-ray diffraction with a diamond-anvil cell u
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::456f40777f33657cab80550ba4d5af43
https://doi.org/10.2138/am.2005.1768
https://doi.org/10.2138/am.2005.1768
Autor:
Francesco P. Sassi, Charles V. Guidotti, James G. Blencoe, Pier Francesco Zanazzi, Paola Comodi
Publikováno v:
Scopus-Elsevier
Plusieurs chercheurs se sont penches sur les mecanismes de transformation d'un shale en ardoise, furent-ils mecaniques, physiques ou chimiques. Nous considerons ici certains aspects qui ont echappe aux auteursanterieurs. Plus precisement, nous evaluo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0b32b58d15a33db57f4ec8c21c7e2f8a
https://doi.org/10.2113/gscanmin.43.1.311
https://doi.org/10.2113/gscanmin.43.1.311
Publikováno v:
Scopus-Elsevier
The structural behavior of phlogopite was studied by in situ single-crystal X-ray diffraction (XRD) in a diamond-anvil cell, using crystals of composition [(K0.91Na0.02Ba0.03) (Fe2+ 0.65Fe3+ 0.163Al0.123Mg1.81 Ti0.149)Si2.708Al1.292O10OH1.725F0.175].
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4e232e34478b7246e0d00abe4537901b
https://doi.org/10.2138/am-2004-0420
https://doi.org/10.2138/am-2004-0420
Publikováno v:
Contributions to Mineralogy and Petrology. 145:578-584
Optically homogeneous augite xenocrysts, closely associated with spinel–peridotite nodules, occur in alkali basalts from Hannuoba (Hebei province, China). They were studied by electron and X-ray diffraction to define the occurrence and significance
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ce56b2fac6db1b8ca82bfb8592512ed6
https://doi.org/10.1007/s00410-003-0467-9
https://doi.org/10.1007/s00410-003-0467-9
Publikováno v:
European Journal of Mineralogy. 15:247-255
The structural behaviour of bikitaite, Li 2 (Al 2 Si 4 O 12 ). 2H 2 O, was investigated under hydrostatic pressure using X-ray single-crystal diffraction data. A Merrill-Bassett diamond anvil cell was mounted with glycerol, as non penetrating pressur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e7221c941ba577f4fb6aef402def0db1
https://doi.org/10.1127/0935-1221/2003/0015-0247
https://doi.org/10.1127/0935-1221/2003/0015-0247