Microscale sealed vessel (MSSV) technique in petroleum systems: a review

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Microscale sealed vessel (MSSV) technique in petroleum systems: a review

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Initial insights into releasing bound biomarkers from kerogen matrices using microscale sealed vessel catalytic hydrogenation (MSSV-HY)
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Thermal release of nitrogen organics from natural organic matter using micro scale sealed vessel pyrolysis
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Carbon isotopic composition of individual hydrocarbons and associated gases evolved from micro-scale sealed vessel (MSSV) pyrolysis of high molecular weight organic material
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Carbon isotopic composition of individual hydrocarbons and associated gases evolved from micro-scale sealed vessel (MSSV) pyrolysis of high molecular weight organic material

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The decomposition of posidonia shale and green river shale kerogens using microscale sealed vessel (MSSV) pyrolysis
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Enhanced late gas generation potential of petroleum source rocks via recombination reactions: Evidence from the Norwegian North Sea
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Biomarker and isotopic signatures of an early Cambrian Lagerstätte in the Stansbury Basin, South Australia
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Biomarker and isotopic signatures of an early Cambrian Lagerstätte in the Stansbury Basin, South Australia

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Kinetics of petroleum generation by programmed-temperature closed-versus open-system pyrolysis
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Kinetics of petroleum generation by programmed-temperature closed-versus open-system pyrolysis

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Molecular hydrogen (H2) and light hydrocarbon gases generation from marine and lacustrine source rocks during closed-system laboratory pyrolysis experiments
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Bacterial biomarkers thermally released from dissolved organic matter
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Hydrocarbon Generation Kinetics of Lacustrine Yanchang Shale in Southeast Ordos Basin, North China
  • Aug 29, 2014
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The upper Triassic Yanchang shale in Southeast Ordos Basin (SOB) is a main potential source rock for conventional petroleum fields and has been recently recognized as an important unconventional reservoir. Here, we report on the hydrocarbon potential of this lacustrine shale using bulk and quantitative pyrolysis techniques. The rock samples were taken from the Chang7 and Chang9 intervals of upper Triassic-aged cores. The analytical program included total organic carbon (TOC), Rock-Eval, pyrolysis gas chromatography (Py–GC), source rock analyzer (SRA), and microscale sealed vessel (MSSV) pyrolysis. Phase kinetic modeling was also employed on the basis of these data sets. The results were used to determine the petroleum-type organofacies, bulk hydrocarbon composition during maturation, bulk and compositional kinetics, and phase behavior of fluids generated in the Yanchang shales. The shales proved to contain type II2 kerogen with organic matter in high abundance and generate paraffinic–naphthenic–aromatic (...

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Evaluating kerogen type according to source quality, compositional heterogeneity and thermal lability
  • Oct 1, 1990
  • Review of Palaeobotany and Palynology
  • B Horsfield

Evaluating kerogen type according to source quality, compositional heterogeneity and thermal lability

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  • Cite Count Icon 48
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Origin of low-molecular-weight alkylthiophenes in pyrolysates of sulphur-rich kerogens as revealed by micro-scale sealed vessel pyrolysis
  • Dec 1, 1998
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Origin of low-molecular-weight alkylthiophenes in pyrolysates of sulphur-rich kerogens as revealed by micro-scale sealed vessel pyrolysis

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  • 10.1016/j.jaap.2013.05.002
Analytical pyrolysis for determining the molecular composition of contemporary monosulfidic black ooze
  • May 13, 2013
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Analytical pyrolysis for determining the molecular composition of contemporary monosulfidic black ooze

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  • 10.1016/j.coal.2017.11.001
Liberation of hydrogen-containing gases during closed system pyrolysis of immature organic matter-rich shales
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  • International Journal of Coal Geology
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Liberation of hydrogen-containing gases during closed system pyrolysis of immature organic matter-rich shales

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Origin of natural gas in the Turpan-Hami Basin, NW China: Evidence from pyrolytic simulation experiment
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  • International Journal of Coal Geology
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Origin of natural gas in the Turpan-Hami Basin, NW China: Evidence from pyrolytic simulation experiment

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