Paleoenvironment of the Eocene Eckfeld Maar lake (Germany): Implication from geochemical analysis of the oil shale sequence
Research output: Contribution to journal › Article › Research › peer-review
Standard
Paleoenvironment of the Eocene Eckfeld Maar lake (Germany): Implication from geochemical analysis of the oil shale sequence. / Sabel, M.; Bechtel, Achim; Püttmann, W. et al.
In: Organic geochemistry, Vol. 36, 2005, p. 873-891.
In: Organic geochemistry, Vol. 36, 2005, p. 873-891.
Research output: Contribution to journal › Article › Research › peer-review
Harvard
Sabel, M, Bechtel, A, Püttmann, W & Hoernes, S 2005, 'Paleoenvironment of the Eocene Eckfeld Maar lake (Germany): Implication from geochemical analysis of the oil shale sequence', Organic geochemistry, vol. 36, pp. 873-891.
APA
Sabel, M., Bechtel, A., Püttmann, W., & Hoernes, S. (2005). Paleoenvironment of the Eocene Eckfeld Maar lake (Germany): Implication from geochemical analysis of the oil shale sequence. Organic geochemistry, 36, 873-891.
Vancouver
Sabel M, Bechtel A, Püttmann W, Hoernes S. Paleoenvironment of the Eocene Eckfeld Maar lake (Germany): Implication from geochemical analysis of the oil shale sequence. Organic geochemistry. 2005;36:873-891.
Author
Bibtex - Download
@article{d451456a003746f6b14fa535f6a66784,
title = "Paleoenvironment of the Eocene Eckfeld Maar lake (Germany): Implication from geochemical analysis of the oil shale sequence",
author = "M. Sabel and Achim Bechtel and W. P{\"u}ttmann and S. Hoernes",
year = "2005",
language = "English",
volume = "36",
pages = "873--891",
journal = "Organic geochemistry",
issn = "0146-6380",
publisher = "Elsevier",
}
RIS (suitable for import to EndNote) - Download
TY - JOUR
T1 - Paleoenvironment of the Eocene Eckfeld Maar lake (Germany): Implication from geochemical analysis of the oil shale sequence
AU - Sabel, M.
AU - Bechtel, Achim
AU - Püttmann, W.
AU - Hoernes, S.
PY - 2005
Y1 - 2005
M3 - Article
VL - 36
SP - 873
EP - 891
JO - Organic geochemistry
JF - Organic geochemistry
SN - 0146-6380
ER -
