Pregled bibliografske jedinice broj: 444363
Preservation of the samarskite structure in a metamict ABO4 mineral: a key to crystal structure identification
Preservation of the samarskite structure in a metamict ABO4 mineral: a key to crystal structure identification // European journal of mineralogy, 22 (2010), 3; 435-442 doi:10.1127/0935-1221/2010/0022-2032 (međunarodna recenzija, članak, znanstveni)
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Naslov
Preservation of the samarskite structure in a metamict ABO4 mineral: a key to crystal structure identification
Autori
Tomašić, Nenad ; Gajović, Andreja ; Bermanec, Vladimir ; Rajić Linarić, Maša ; Su, Dangsheng ; Škoda, Radek
Izvornik
European journal of mineralogy (0935-1221) 22
(2010), 3;
435-442
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
samarskite ; low-temperature modification ; metamictisation ; pre-metamict structure ; TEM
Sažetak
Relics of the original samarskite structure were identified in a metamict ABO4 mineral from Beinmyr pegmatite, Norway, using selected area electron diffraction (SAED) and high-resolution transmission electron microscopy (HRTEM). The chemical composition of the sample confirmed the affiliation to the samarskite group giving general formula (REE0.322Ca0.269Fe0.231U0.142Mn0.031Pb0.011Th0.010Zr0.010Al0.004Sc0.002 Na0.001K0.001)1.034(Nb0.707Ta0.267Ti0.069W0.017Sn0.007)1.067O4. The structure identified by transmission electron microscopy (TEM) techniques is well related to the proposed low-temperature samarskite modification (Sugitani et al. 1985) crystallising orthorhombically with the cell parameters a=5.68(1) Å, b=4.94(1) Å, c=5.24(2) Å. The observed diffraction maxima conform well to Pbcn space group. The original mineral sample showed to be X-ray amorphous. Gradual recrystallisation in air in the temperature range between 400 and 1000 °C yielded a pyrochlore phase being stable at all experimental temperatures. At 800 °C a high-temperature samarskite phase (s. g. P2/c) co-crystallised with an increase in crystallinity at 1000 °C. Recrystallisation in a reducing atmosphere (Ar/H2) did not yield the high-temperature samarskite phase solely. Unsuccessful recrystallisation of the high-temperature samarskite modification is mainly related to an alteration which shifted the composition of samarskite to pyrochlore as evidenced by occurrence of altered domains in the sample.
Izvorni jezik
Engleski
Znanstvena područja
Fizika, Geologija, Kemija
POVEZANOST RADA
Projekti:
098-0982934-2742 - Nanočestice u biogeokemijskim procesima u okolišu
098-0982904-2898 - Fizika i primjena nanostruktura i volumne tvari (Ivanda, Mile, MZOS ) ( CroRIS)
098-0982934-2715 - Biogeokemija metala u sedimentacijskim sustavima i tlima Hrvatske (Kniewald, Goran, MZOS ) ( CroRIS)
119-0000000-1158 - Međudjelovanje minerala i okoliša (Bermanec, Vladimir, MZOS ) ( CroRIS)
Ustanove:
Institut "Ruđer Bošković", Zagreb,
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Andreja Gajović
(autor)
Maša Rajić Linarić
(autor)
Vladimir Bermanec
(autor)
Nenad Tomašić
(autor)
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus