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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
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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.
@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},
}

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