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Preliminary data on the crystal-chemical characteristics of beryl from Cer Mt. (Serbia)

Samo za registrovane korisnike
2010
Autori
Tančić, Pavle
Poznanović, Maja
Dimitrijević, Radovan
Konferencijski prilog (Objavljena verzija)
Metapodaci
Prikaz svih podataka o dokumentu
Apstrakt
A beryl crystal from Cer Mt. (Serbia) studied in this paper was characterized by means of XRPD and wet-chemical analyses. It has following unit cell dimensions: a = 9.2166(8) Å, c = 9.192(1) Å, V = 676.2(1) Å3 and ratio c/a = 0.9973. According to the calculated c/a ratio and structural formula of (Be2.86Li0.11)2.97(Al1.96Fe2+0.05)2.01Si5.96O18(Na0.09Ca0.03 Mg0.03K0.01)0.16 × 0.14H2O composition, this sample belongs to the “normal beryl group”. The obtained characteristics prove that the host pegmatite is of Li-bearing type.
Ključne reči:
crystallography / beryl
Izvor:
Abstracts volume - XIX CBGA Congress, Geologica Balcanica, 2010, 39, 1-2, 384-
Izdavač:
  • Carpathian-Balkan Geological Association
Napomena:
  • Paper: https://cer.ihtm.bg.ac.rs/handle/123456789/5973
Povezane informacije:
  • Povezani sadržaj
    https://cer.ihtm.bg.ac.rs/handle/123456789/5973

ISSN: 0324-0894

[ Google Scholar ]
Handle
https://hdl.handle.net/21.15107/rcub_cer_6017
URI
https://cer.ihtm.bg.ac.rs/handle/123456789/6017
Kolekcije
  • Radovi istraživača pre dolaska u IHTM / Researchers' papers before joining ICTM
Institucija/grupa
IHTM
TY  - CONF
AU  - Tančić, Pavle
AU  - Poznanović, Maja
AU  - Dimitrijević, Radovan
PY  - 2010
UR  - https://cer.ihtm.bg.ac.rs/handle/123456789/6017
AB  - A beryl crystal from Cer Mt. (Serbia) studied in this paper was characterized by means of XRPD and wet-chemical analyses. It has following unit cell dimensions: a = 9.2166(8) Å, c = 9.192(1) Å, V = 676.2(1) Å3 and ratio c/a = 0.9973. According to the calculated c/a ratio and structural formula of (Be2.86Li0.11)2.97(Al1.96Fe2+0.05)2.01Si5.96O18(Na0.09Ca0.03 Mg0.03K0.01)0.16 × 0.14H2O composition, this sample belongs to the “normal beryl group”. The obtained characteristics prove that the host pegmatite is of Li-bearing type.
PB  - Carpathian-Balkan Geological Association
C3  - Abstracts volume - XIX CBGA Congress, Geologica Balcanica
T1  - Preliminary data on the crystal-chemical characteristics of beryl from Cer Mt. (Serbia)
VL  - 39
IS  - 1-2
SP  - 384
UR  - https://hdl.handle.net/21.15107/rcub_cer_6017
ER  - 
@conference{
author = "Tančić, Pavle and Poznanović, Maja and Dimitrijević, Radovan",
year = "2010",
abstract = "A beryl crystal from Cer Mt. (Serbia) studied in this paper was characterized by means of XRPD and wet-chemical analyses. It has following unit cell dimensions: a = 9.2166(8) Å, c = 9.192(1) Å, V = 676.2(1) Å3 and ratio c/a = 0.9973. According to the calculated c/a ratio and structural formula of (Be2.86Li0.11)2.97(Al1.96Fe2+0.05)2.01Si5.96O18(Na0.09Ca0.03 Mg0.03K0.01)0.16 × 0.14H2O composition, this sample belongs to the “normal beryl group”. The obtained characteristics prove that the host pegmatite is of Li-bearing type.",
publisher = "Carpathian-Balkan Geological Association",
journal = "Abstracts volume - XIX CBGA Congress, Geologica Balcanica",
title = "Preliminary data on the crystal-chemical characteristics of beryl from Cer Mt. (Serbia)",
volume = "39",
number = "1-2",
pages = "384",
url = "https://hdl.handle.net/21.15107/rcub_cer_6017"
}
Tančić, P., Poznanović, M.,& Dimitrijević, R.. (2010). Preliminary data on the crystal-chemical characteristics of beryl from Cer Mt. (Serbia). in Abstracts volume - XIX CBGA Congress, Geologica Balcanica
Carpathian-Balkan Geological Association., 39(1-2), 384.
https://hdl.handle.net/21.15107/rcub_cer_6017
Tančić P, Poznanović M, Dimitrijević R. Preliminary data on the crystal-chemical characteristics of beryl from Cer Mt. (Serbia). in Abstracts volume - XIX CBGA Congress, Geologica Balcanica. 2010;39(1-2):384.
https://hdl.handle.net/21.15107/rcub_cer_6017 .
Tančić, Pavle, Poznanović, Maja, Dimitrijević, Radovan, "Preliminary data on the crystal-chemical characteristics of beryl from Cer Mt. (Serbia)" in Abstracts volume - XIX CBGA Congress, Geologica Balcanica, 39, no. 1-2 (2010):384,
https://hdl.handle.net/21.15107/rcub_cer_6017 .

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