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There were two main stages of hydrocarbon generation and expulsion of oil from the major hydrocarbon source rocks.
The major hydrocarbon source rocks in the PLP marine carbonate giant oil and gas fields are mainly shales of considerable thickness.
The formation is predominantly overpressured and is the major hydrocarbon source rock in the basin while the paralic shore face sands of the Agbada Formation are the major reservoirs.
The hydrocarbon charge history of the Paleogene in the northern Dongpu Depression was analyzed in detail based on a comprehensive analysis of the generation and expulsion history of the major hydrocarbon source rocks, fluorescence microscopic features and fluid inclusion petrography.
The hydrocarbon charge stages were divided qualitatively based on the analysis of generation and expulsion stages of major hydrocarbon source rocks and fluorescence microscopic features (Jarmołowicz-Szulc et al. 2012); the hydrocarbon fluid inclusion forming periods were divided according to the diagenetic evolution sequence of host minerals combined with reservoir burial evolution history.
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Three major types of hydrocarbon sources exist: insoluble, soluble, and acid-soluble organic matter.
The Shahejie Formation (Es) in the Western Depression are not only the most important source rocks responsible for the major hydrocarbon accumulations, they are also the major reservoir rocks.
Ammonia production requires hydrogen from a hydrocarbon source.
Abnormally high pressures commonly exist in the gas reservoirs in foreland basins where multiple sets of source reservoir seal combinations are present, and the major trap type is the anticlinal trap type and faults are the major hydrocarbon migration pathways.
This makes finding major hydrocarbon deposits there unlikely.
The hydrocarbons in hydrocarbon source rocks can be entirely expelled within the effective thickness of hydrocarbon expulsion.
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