Carbon and oxygen isotope composition of Lower Palaeozoic limestones and concretions: an example of high temperature diagenesis
Research output: Contribution to journal › Journal article › Research › peer-review
Standard
Carbon and oxygen isotope composition of Lower Palaeozoic limestones and concretions : an example of high temperature diagenesis. / Buchardt, Bjørn.
In: Terra Cognita, Vol. 4, 1984, p. 37-38.Research output: Contribution to journal › Journal article › Research › peer-review
Harvard
Buchardt, B 1984, 'Carbon and oxygen isotope composition of Lower Palaeozoic limestones and concretions: an example of high temperature diagenesis', Terra Cognita, vol. 4, pp. 37-38.
APA
Buchardt, B. (1984). Carbon and oxygen isotope composition of Lower Palaeozoic limestones and concretions: an example of high temperature diagenesis. Terra Cognita, 4, 37-38.
Vancouver
Buchardt B. Carbon and oxygen isotope composition of Lower Palaeozoic limestones and concretions: an example of high temperature diagenesis. Terra Cognita. 1984;4:37-38.
Author
Bibtex
@article{db4500104b7611de87b8000ea68e967b,
title = "Carbon and oxygen isotope composition of Lower Palaeozoic limestones and concretions: an example of high temperature diagenesis",
author = "Bj{\o}rn Buchardt",
year = "1984",
language = "English",
volume = "4",
pages = "37--38",
journal = "Terra Cognita",
}
RIS
TY - JOUR
T1 - Carbon and oxygen isotope composition of Lower Palaeozoic limestones and concretions
T2 - an example of high temperature diagenesis
AU - Buchardt, Bjørn
PY - 1984
Y1 - 1984
M3 - Journal article
VL - 4
SP - 37
EP - 38
JO - Terra Cognita
JF - Terra Cognita
ER -
ID: 12412666