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The Fe2+ quadrupole splitting at octahedral sites in chain silicates: Correlations with the site-distortion parameters.

L ZHE and Eddy De Grave UGent (1998) HYPERFINE INTERACTIONS. 116(1-4). p.173-178
Please use this url to cite or link to this publication:
author
organization
year
type
journalArticle (original)
publication status
published
subject
journal title
HYPERFINE INTERACTIONS
Hyperfine Interact.
volume
116
issue
1-4
pages
173-178 pages
Web of Science type
Article
Web of Science id
000077312800016
ISSN
0304-3843
language
English
UGent publication?
yes
classification
A1
id
181002
handle
http://hdl.handle.net/1854/LU-181002
date created
2004-01-14 13:41:00
date last changed
2016-12-19 15:38:46
@article{181002,
  author       = {ZHE, L and De Grave, Eddy},
  issn         = {0304-3843},
  journal      = {HYPERFINE INTERACTIONS},
  language     = {eng},
  number       = {1-4},
  pages        = {173--178},
  title        = {The Fe2+ quadrupole splitting at octahedral sites in chain silicates: Correlations with the site-distortion parameters.},
  volume       = {116},
  year         = {1998},
}

Chicago
ZHE, L, and Eddy De Grave. 1998. “The Fe2+ Quadrupole Splitting at Octahedral Sites in Chain Silicates: Correlations with the Site-distortion Parameters.” Hyperfine Interactions 116 (1-4): 173–178.
APA
ZHE, L., & De Grave, E. (1998). The Fe2+ quadrupole splitting at octahedral sites in chain silicates: Correlations with the site-distortion parameters. HYPERFINE INTERACTIONS, 116(1-4), 173–178.
Vancouver
1.
ZHE L, De Grave E. The Fe2+ quadrupole splitting at octahedral sites in chain silicates: Correlations with the site-distortion parameters. HYPERFINE INTERACTIONS. 1998;116(1-4):173–8.
MLA
ZHE, L, and Eddy De Grave. “The Fe2+ Quadrupole Splitting at Octahedral Sites in Chain Silicates: Correlations with the Site-distortion Parameters.” HYPERFINE INTERACTIONS 116.1-4 (1998): 173–178. Print.