The crystal structure of natural gugiaite, Ca2BeSi2O7

Citation
Zm. Yang et al., The crystal structure of natural gugiaite, Ca2BeSi2O7, N J MINER M, (4), 2001, pp. 186-192
Citations number
12
Categorie Soggetti
Earth Sciences
Journal title
NEUES JAHRBUCH FUR MINERALOGIE-MONATSHEFTE
ISSN journal
00283649 → ACNP
Issue
4
Year of publication
2001
Pages
186 - 192
Database
ISI
SICI code
0028-3649(200104):4<186:TCSONG>2.0.ZU;2-B
Abstract
The crystal structure of the original natural gugiaite, Ca2BeSi2O7, from th e skarn rocks in the Gugia alkaline complex, Liaoning Province, China, is d etermined from CCD data in space group P (4) over bar2(1)m, n = 7.4330(10), c = 4.9970(10) Angstrom, V = 276.08(8) Angstrom (3), Z = 2. The structure is basically consistent with that of the synthetic one, although there are longer Be-O distances, smaller distortions of BeO4 tetrahedron and larger d istortions of SiO4 tetrahedron than those in synthetic one.