Lithology and Source Rock Generative Potential of the Eggerding Formation (Lower Oligocene, Molasse Basin)
Research output: Thesis › Master's Thesis
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Abstract
The Lower Oligocene in the Molasse basin is divided from bottom to top into Schöneck, Dynow, Eggerding and Zupfing formations. The Eggerding Formation, about 40 m thick, consists in its lower part of shaly marlstone with up to 6.0% organic carbon (TOC) and white bands, which are rich in coccolithophorides. The upper part of the Eggerding Formation consists of a homogenous sequence of marly shale with about 1.65% TOC. Calcite and TOC contents in the Zupfing Formation are about 30% and
Details
Translated title of the contribution | Lithologie und Muttergesteins-Potential der Eggerding-Formation (Unteroligozän, Molasse Becken) |
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Original language | English |
Qualification | Dipl.-Ing. |
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Award date | 19 Dec 2008 |
Publication status | Published - 2008 |