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Kerogen concentrates as well as whole rock samples of the Lower Jurassic Posidonia Shale, representing a complete maturity series from immature to highly overmature, were analyzed using organic petrography, palynology, bulk geochemical analysis, FT-IR and Curie Point-Pyrolysis-GC–MS (CP-Py-GC–MS) in order to investigate changes in kerogen composition with increasing maturation. Vitrinite reflectance...
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