Zobrazeno 1 - 10
of 45
pro vyhledávání: '"Fabien Cesbron"'
Autor:
Dominique Lapraz, Daniel Ohnenstetter, Fabien Cesbron, Alain Baumer, Gérard Panczer, H. Prevost, Philippe Blanc
Publikováno v:
Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science. 329:629-635
Comparative study of luminescence properties of doped synthetic minerals (anhydrite, calcite, fluorite and zircon) by cathodoluminescence and fluorescence methods is presented. The Eu 3+ doped minerals (anhydrite; other sulfates; fluorite) exhibit pa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::96326037fc0587ec61e3eaf1d71185c5
https://doi.org/10.1016/s1251-8050(00)87639-9
https://doi.org/10.1016/s1251-8050(00)87639-9
Publikováno v:
Mineralogical Magazine. 57:301-308
Uranyl-silicates are widespread minerals in oxidised parts of various uranium deposits, and they frequently contain associations of the polymorphic forms of uranophane. In several recent works devoted to the study of uranium deposits as natural analo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::faffc505e2a86f26ff3964bced10e8dc
https://doi.org/10.1180/minmag.1993.057.387.12
https://doi.org/10.1180/minmag.1993.057.387.12
Autor:
Guy Rémond, Gérard Panczer, Alain Baumer, Fabien Cesbron, Phillipe Blanc, Daniel Ohnenstetter
Publikováno v:
Cathodoluminescence in Geosciences ISBN: 9783642085260
As the geochemical behavior of the rare earth elements (REE) is of increasing interest in geology (see the reviews edited by Lipin and McKay 1989 and Jones et al. 1996), the main REE minerals in most igneous, metamorphic and sedimentary rocks are now
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::71b35a2a02a52f8c42f5515b98e5af72
https://doi.org/10.1007/978-3-662-04086-7_5
https://doi.org/10.1007/978-3-662-04086-7_5
Publikováno v:
Bulletin de Minéralogie. 103:122-128
Triclinic, P[-1], a = 8.440 (8.459), b = 7.608 (7.613), c = 6.958 (6.968) Å, α = 82.32° (82.21°), β = 98.30° (98.25°), γ = 95.53° (95.86°), V = 436.8 (438.6)ų, Z = 2. Catti et al. (1980) describe its structure. The strongest lines in pow
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1a6453f0b90f6ea89e03004acc371608
https://doi.org/10.3406/bulmi.1980.7384
https://doi.org/10.3406/bulmi.1980.7384
Publikováno v:
European Journal of Mineralogy. 1:127-134
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::456d61a0ae98d03b9682f5e21109bc59
https://doi.org/10.1127/ejm/01/1/0127
https://doi.org/10.1127/ejm/01/1/0127
Autor:
Fabien Cesbron
Publikováno v:
Bulletin de Minéralogie. 110:111-117
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1f777cfb228c52dbfec4c18b975569dc
https://doi.org/10.3406/bulmi.1987.8029
https://doi.org/10.3406/bulmi.1987.8029
Autor:
Fabien Cesbron, Roland Pierrot
Publikováno v:
Bulletin de Minéralogie. 101:107-113
Cesbron Fabien, Pierrot Roland. Les espèces minérales décrites dans le Bulletin de la Société de 1878 à 1978. In: Bulletin de Minéralogie, volume 101, 2, 1978. 1878-1978, centenaire de la Société Française de Minéralogie et Cristallographi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2ad895b7e61c6f18c3bd1ce56d9a99af
https://doi.org/10.3406/bulmi.1978.7178
https://doi.org/10.3406/bulmi.1978.7178
Publikováno v:
Analytica Chimica Acta. 98:299-306
Resume Des concentrations en brome de 0,6–120 mg l −1 peuvent etre determinees directement sur liquide par fluorescence x en utilisant le selenium comme etalon interne pour eliminer les effets d'interference; pour de plus faibles concentrations i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a573c97f5fd83f0fde965dc0105e22e
https://doi.org/10.1016/s0003-2670(01)84058-7
https://doi.org/10.1016/s0003-2670(01)84058-7
Autor:
Alexandre Kosakevitch, Fabien Cesbron
Publikováno v:
Bulletin de Minéralogie. 108:859-869
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a43e8f9d54ff740624745574b7282d6e
https://doi.org/10.3406/bulmi.1985.7907
https://doi.org/10.3406/bulmi.1985.7907
Publikováno v:
Bulletin de Minéralogie. 108:825-828
A tabular zircon, with dominant {001} pinacoid, was observed in the sodium-rich pyroxene syenites of the Meponda alkaline complex, Mozambique. Comparison of its morphology with those of zircon crystals from several alkaline granites — Cameroun, Nig
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0f6b9abebb3094378ca6679a2815a886
https://doi.org/10.3406/bulmi.1985.7900
https://doi.org/10.3406/bulmi.1985.7900