TY - THES

T1 - Lithology and Source Rock Generative Potential of the Eggerding Formation (Lower Oligocene, Molasse Basin)

AU - Leitner, Birgit

N1 - embargoed until null

PY - 2008

Y1 - 2008

N2 - 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

AB - 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

KW - Lower Oligocene Molasse Basin Eggerding Formation Source rock potential Leco Rock-Eval Log measurements Coccolithophorides

KW - Unteroligozän Molasse Becken Eggerding-Formation Muttergesteins-Potential Leco Rock Eval Biomarkeranalyse Bohrlochmessungen Coccolithophoriden

M3 - Master's Thesis

ER -