Carbon and oxygen isotope composition of Lower Palaeozoic limestones and concretions: an example of high temperature diagenesis

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Standard

Carbon and oxygen isotope composition of Lower Palaeozoic limestones and concretions : an example of high temperature diagenesis. / Buchardt, Bjørn.

I: Terra Cognita, Bind 4, 1984, s. 37-38.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Buchardt, B 1984, 'Carbon and oxygen isotope composition of Lower Palaeozoic limestones and concretions: an example of high temperature diagenesis', Terra Cognita, bind 4, s. 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

Buchardt, Bjørn. / Carbon and oxygen isotope composition of Lower Palaeozoic limestones and concretions : an example of high temperature diagenesis. I: Terra Cognita. 1984 ; Bind 4. s. 37-38.

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