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Journal Article

Carbon dioxide in the Rhenish Massif.

Plateau uplift: the Rhenish Shield - a case history (1983) 152
DOI: 10.1007/978-3-642-69219-2_22
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Abstract

Carbon dioxide of the order of 0.5-1 X 106 t/yr emerges from the whole Eifel region. Carbon isotope studies indicate a magmatic source; locally, isotopic alteration is caused by kinetic fractionation in unsaturated water bodies.-J.M.H.

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APA

Puchelt, H. (1983). Carbon dioxide in the Rhenish Massif. Plateau Uplift: The Rhenish Shield - a Case History, 152. https://doi.org/10.1007/978-3-642-69219-2_22

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