Standard
Cordierite-anorthoclase hornfels xenoliths in metamorphic aureole. / Renzulli, Albert; Tribaudino, M.; Salvioli-Mariani, E; Serri, Giancarlo; Holm, Paul Martin.
I:
European Journal of Mineralogy, Nr. 15, 2003, s. 665-680.
Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
Harvard
Renzulli, A, Tribaudino, M, Salvioli-Mariani, E, Serri, G & Holm, PM 2003, 'Cordierite-anorthoclase hornfels xenoliths in metamorphic aureole', European Journal of Mineralogy, nr. 15, s. 665-680.
APA
Renzulli, A., Tribaudino, M., Salvioli-Mariani, E., Serri, G., & Holm, P. M. (2003). Cordierite-anorthoclase hornfels xenoliths in metamorphic aureole. European Journal of Mineralogy, (15), 665-680.
Vancouver
Renzulli A, Tribaudino M, Salvioli-Mariani E, Serri G, Holm PM. Cordierite-anorthoclase hornfels xenoliths in metamorphic aureole. European Journal of Mineralogy. 2003;(15):665-680.
Author
Renzulli, Albert ; Tribaudino, M. ; Salvioli-Mariani, E ; Serri, Giancarlo ; Holm, Paul Martin. / Cordierite-anorthoclase hornfels xenoliths in metamorphic aureole. I: European Journal of Mineralogy. 2003 ; Nr. 15. s. 665-680.
Bibtex
@article{9d362af074bf11dbbee902004c4f4f50,
title = "Cordierite-anorthoclase hornfels xenoliths in metamorphic aureole",
abstract = "xenoliths, aureole, petrology",
author = "Albert Renzulli and M. Tribaudino and E Salvioli-Mariani and Giancarlo Serri and Holm, {Paul Martin}",
year = "2003",
language = "English",
pages = "665--680",
journal = "European Journal of Mineralogy",
issn = "0935-1221",
publisher = "E.Schweizerbart'sche Verlagsbuchhandlung",
number = "15",
}
RIS
TY - JOUR
T1 - Cordierite-anorthoclase hornfels xenoliths in metamorphic aureole
AU - Renzulli, Albert
AU - Tribaudino, M.
AU - Salvioli-Mariani, E
AU - Serri, Giancarlo
AU - Holm, Paul Martin
PY - 2003
Y1 - 2003
N2 - xenoliths, aureole, petrology
AB - xenoliths, aureole, petrology
M3 - Journal article
SP - 665
EP - 680
JO - European Journal of Mineralogy
JF - European Journal of Mineralogy
SN - 0935-1221
IS - 15
ER -
