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Temperature dependence of the hyperfine parameters of synthetic P2(1)/c Mg-Fe clinopyroxenes along the MgSiO3-FeSiO3 join.

Sigrid Eeckhout, Eddy De Grave UGent, CA MCCAMMON and Renaud Vochten (2000) AMERICAN MINERALOGIST. 85(7-8). p.943-952
Please use this url to cite or link to this publication:
author
organization
year
type
journalArticle (original)
publication status
published
subject
journal title
AMERICAN MINERALOGIST
Am. Miner.
volume
85
issue
7-8
pages
943-952 pages
Web of Science type
Article
Web of Science id
000087965500008
ISSN
0003-004X
language
English
UGent publication?
yes
classification
A1
id
124122
handle
http://hdl.handle.net/1854/LU-124122
date created
2004-01-14 13:36:00
date last changed
2016-12-19 15:37:49
@article{124122,
  author       = {Eeckhout, Sigrid and De Grave, Eddy and MCCAMMON, CA and Vochten, Renaud},
  issn         = {0003-004X},
  journal      = {AMERICAN MINERALOGIST},
  language     = {eng},
  number       = {7-8},
  pages        = {943--952},
  title        = {Temperature dependence of the hyperfine parameters of synthetic P2(1)/c Mg-Fe clinopyroxenes along the MgSiO3-FeSiO3 join.},
  volume       = {85},
  year         = {2000},
}

Chicago
Eeckhout, Sigrid, Eddy De Grave, CA MCCAMMON, and Renaud Vochten. 2000. “Temperature Dependence of the Hyperfine Parameters of Synthetic P2(1)/c Mg-Fe Clinopyroxenes Along the MgSiO3-FeSiO3 Join.” American Mineralogist 85 (7-8): 943–952.
APA
Eeckhout, Sigrid, De Grave, E., MCCAMMON, C., & Vochten, R. (2000). Temperature dependence of the hyperfine parameters of synthetic P2(1)/c Mg-Fe clinopyroxenes along the MgSiO3-FeSiO3 join. AMERICAN MINERALOGIST, 85(7-8), 943–952.
Vancouver
1.
Eeckhout S, De Grave E, MCCAMMON C, Vochten R. Temperature dependence of the hyperfine parameters of synthetic P2(1)/c Mg-Fe clinopyroxenes along the MgSiO3-FeSiO3 join. AMERICAN MINERALOGIST. 2000;85(7-8):943–52.
MLA
Eeckhout, Sigrid, Eddy De Grave, CA MCCAMMON, et al. “Temperature Dependence of the Hyperfine Parameters of Synthetic P2(1)/c Mg-Fe Clinopyroxenes Along the MgSiO3-FeSiO3 Join.” AMERICAN MINERALOGIST 85.7-8 (2000): 943–952. Print.