2020
New crystal-chemical data on zincoberaunite from Krásno near Horní Slavkov (Czech Republic)
TVRDÝ, Jaromír, Jakub PLÁŠIL a Radek ŠKODAZákladní údaje
Originální název
New crystal-chemical data on zincoberaunite from Krásno near Horní Slavkov (Czech Republic)
Autoři
TVRDÝ, Jaromír (203 Česká republika, garant, domácí), Jakub PLÁŠIL (203 Česká republika) a Radek ŠKODA (203 Česká republika, domácí)
Vydání
Journal of Geosciences, Czech Geological Society, 2020, 1802-6222
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10504 Mineralogy
Stát vydavatele
Česká republika
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 1.525
Kód RIV
RIV/00216224:14310/20:00115539
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000525954600006
Klíčová slova anglicky
zincoberaunite; phosphate; crystal structure; Raman spectra; Krásno near Horní Slavkov; Czech Republic
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 30. 11. 2020 11:05, Mgr. Marie Šípková, DiS.
Anotace
V originále
A study of zincoberaunite from Krásno near Horní Slavkov (Czech Republic) provided new chemical and structural data of this rare member of the beraunite group. The studied material is monoclinic, space group C2/c. Based on refined site occupancies and bond-valence considerations, the structural formula is (Zn0.81Al0.19)(OH)2(Fe0.61Al0.39)(OH)2(H2O)2(Fe1.52Al0.48)(H2O)2(Fe1.72Al0.28)(OH)(PO4)3.83(AsO4)0.17(H2O)2. Electron-microprobe analyses support the obtained results. However, keeping the same cation occupancy at the M2–M4 sites, the ratio of Al3+ to Me2+ at the M1 site requires the presence of divalent cations as follows: (Zn0.57Fe0.24Al0.19)1.00(Fe3.85Al1.15)5.00[(PO4)3.89(AsO4)0.10(SiO4)0.01]4.00[(OH)4.59F0.24 O0.17]5.00(OH2)4.00·2H2O. Individual prismatic zincoberaunite crystals exhibit a chemical zonation manifested by increasing Fe and decreasing Zn and Al contents from cores to rims. The mineral composition is close to the Zn–Al-rich members of the beraunite group known from the same locality, but in this case, dominant occupancy of Zn at the M1 site was confirmed. With its increased aluminium content, zincoberaunite from Krásno differs significantly from the holotype specimen described from Hagendorf South pegmatite in Germany. The most prominent Raman bands are in good agreement with data published for related members of the beraunite group. Structure refinement (R = 3.56 % for 1906 observed unique reflections) revealed three different types of OH or H2O, which play distinct role in structure bonding.
Návaznosti
MUNI/A/1387/2018, interní kód MU |
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