Pregled bibliografske jedinice broj: 101084
Order disorder in hyalophane feldspar: NMR study
Order disorder in hyalophane feldspar: NMR study // 18th General Meeting of the International Mineralogical Association - Programme with abstracts
Edinburgh: International Mineralogical Association, 2002. (poster, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 101084 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Order disorder in hyalophane feldspar: NMR study
Autori
Bermanec, Vladimir ; Sherriff, Barbara L.
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
18th General Meeting of the International Mineralogical Association - Programme with abstracts
/ - Edinburgh : International Mineralogical Association, 2002
Skup
18th General Meeting of the International Mineralogical Association
Mjesto i datum
Edinburgh, Ujedinjeno Kraljevstvo, 01.09.2002. - 06.09.2002
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
hyalophane; NMR spectra
Sažetak
Hyalophane is a Ba rich feldspar which is along the join of orthoclase, celsian and albite. There is no yet published data about NMR of hyalophane or celsian and there is no real data about order disorder within this feldspar. The spectra are interpreted by comparing with papers on alkali feldspar and anorthite (Phillips et al. 1988, 1992 ; Sherriff and Hartman 1985). The interpretation of NMR peaks has caused some difficulty. It was possible to fit four peaks but there may be more than was possible to resolve. Phillips et al. (1992) were able to resolve eight peaks corresponding to the eight crystallographical environments for Si in anorthite. According to de Pieri and Quareni (1977) there are two T sites in both low and high hyalophane. However the spectra are easier to interpret if there are four T sites as in low temperature albite and orthoclase. In accordance with the allocation of peaks for feldspars I would assign these peaks to T1o (-88.4 ppm), T2o (-91.5 ppm), T1m (-95.6 ppm) and T2m (-101.0 ppm). Then the four sites would have a Si occupation of 0.5, 0.6 1.0, and 0.5 respectively. This means that the Al is spread over 3 sites T1o T2o and T2m. Although there are some informations about exholutions within hyalophane (Viswanathan and Kielhorn, 1983 ; Nakano, 1979) in this case there is no evidence for that on the basis of electron microscopy, polarizing microscopy and X-ray diffraction investigations
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
119304
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Vladimir Bermanec
(autor)