reportBiological markers, compounds derived essentially unchanged from living organisms, are found in oil-bearing rocks, petroleum and most ancient sediments. We are investigating the variation in ratios of certain biomarkers in shale oils and their use as tracers for relating oil to source rock during in-situ retorting. We have produced oil samples at 12°C/min from 1- and 2-foot shale composites from three Green River formation cores and have measured the occurrence of several isoprenoid and sterane compounds using capillary gas chromatography of these oils. Because alkene/alkane ratios of most of these compounds depend strongly on pyrolysis temperature and/or heating rate, we use ratios of alkenes plus alkanes that are largely independent...
Hydrocarbons and organic biomarkers extracted from black shales and other carbonaceous sedimentary r...
Oil spills are classified according to chemical types that reflect qualitative and quantitative chan...
Oil-bearing fluid inclusions occur in a ca. 2.45 Ga fluvial metaconglomerate of the Matinenda Format...
reportBiological markers, compounds derived essentially unchanged from living organisms, are found i...
reportIsoprenoid and other hydrocarbons that are formed in living organisms and preserved in ancient...
Lipid biomarkers play an important role in defining oil-source rock correlations. A fundamental assu...
The Lower Huron Shale (Upper Devonian) is considered the largest shale gas reservoir in the Big Sand...
The molecular and isotopic composition of biomarkers in initial bitumen isolated from immature (0.41...
The molecular and isotopic composition of biomarkers in initial bitumen isolated from immature (0.41...
The Lower Huron Shale (Upper Devonian) is considered the largest shale gas reservoir in the Big Sand...
18 pages, 4 figures, 2 tables, 53 references.The application of alkane biomarkers for source, palaeo...
The molecular and isotopic composition of biomarkers in initial bitumen isolated from immature (0.41...
The Neoproterozoic-Early Cambrian time is the cradle of multicellular, eukaryotic life and thereafte...
Molecular fossils record aspects of Neoproterozoic-Early Cambrian palaeobiology in the Bikaner-Nagau...
It is generally accepted that in mature shales, biomarkers and pyrolysis proxies are not very helpfu...
Hydrocarbons and organic biomarkers extracted from black shales and other carbonaceous sedimentary r...
Oil spills are classified according to chemical types that reflect qualitative and quantitative chan...
Oil-bearing fluid inclusions occur in a ca. 2.45 Ga fluvial metaconglomerate of the Matinenda Format...
reportBiological markers, compounds derived essentially unchanged from living organisms, are found i...
reportIsoprenoid and other hydrocarbons that are formed in living organisms and preserved in ancient...
Lipid biomarkers play an important role in defining oil-source rock correlations. A fundamental assu...
The Lower Huron Shale (Upper Devonian) is considered the largest shale gas reservoir in the Big Sand...
The molecular and isotopic composition of biomarkers in initial bitumen isolated from immature (0.41...
The molecular and isotopic composition of biomarkers in initial bitumen isolated from immature (0.41...
The Lower Huron Shale (Upper Devonian) is considered the largest shale gas reservoir in the Big Sand...
18 pages, 4 figures, 2 tables, 53 references.The application of alkane biomarkers for source, palaeo...
The molecular and isotopic composition of biomarkers in initial bitumen isolated from immature (0.41...
The Neoproterozoic-Early Cambrian time is the cradle of multicellular, eukaryotic life and thereafte...
Molecular fossils record aspects of Neoproterozoic-Early Cambrian palaeobiology in the Bikaner-Nagau...
It is generally accepted that in mature shales, biomarkers and pyrolysis proxies are not very helpfu...
Hydrocarbons and organic biomarkers extracted from black shales and other carbonaceous sedimentary r...
Oil spills are classified according to chemical types that reflect qualitative and quantitative chan...
Oil-bearing fluid inclusions occur in a ca. 2.45 Ga fluvial metaconglomerate of the Matinenda Format...