Isotopic characterization of a complete upper jurassic succession. Implications for stratigraphic classification, dolomitization and porosity evolution

Martin Ernst Nowak

Research output: Chapter in Book/Report/Conference proceedingConference contribution

Abstract

We measured and evaluated carbon and oxygen isotopic values of bulk rock samples of the Moosburg drilling core. The data suggest that strata of Oxfordian, Kimmeridgian and Tithonian age can be distinguished according to their carbon and oxygen isotopic values. Dolomites from Kimmeridgian strata and Tithonian strata show significant differences in their oxygen isotopic values, too.
Original languageEnglish (US)
Title of host publicationFirst EAGE Workshop on Geothermal Energy and Hydro Power in Africa
PublisherEuropean Association of Geoscientists & Engineers
ISBN (Print)9789462823747
DOIs
StatePublished - 2020

Bibliographical note

KAUST Repository Item: Exported on 2021-05-12

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