CHARACTERISTICS AND FORMING CONDITIONS OF LAKE-FACIES CARBONATE-ROCK OIL AND GAS POOLS IN THE NANYISHAN STRUCTURE OF THE QAIDAM BASIN
Gan Gui
Abstract
Gan Gui
Abstract
As a typical example of lakefacies carbonaterock oil and gas pools consisted by shallow oil pools and mediumdeep gas condensate pools, Nanyishan oil and gas field in the Qaidam Basin has altogether four sets of hydrocarbon source rocks. The whole stratigraphic profile is dominated by argillite, micritic carbonate rock comes second. The reservoirs of hydrocarbon are carbonate rocks, including argillaceous micritic dolostone, argillaceous micritic limestone, micritic limestone, algal limestone, etc. The storage spaces are mainly intercrystal pores, intergranular pores, solution openings, fissures and karst caves. The reservoirs, which have the thickness of 25m in general, have rather stable plane distribution. Tectonic fractures are all welldeveloped from surface to underground. The clear reducing of seismicwave velocity and abnormal highpressure are observed in the mediumdeep layers of hydrocarbondistributive areas. The fissiontrack testing of fractureinfilling calcite revealed that fractures occurred before the generation and migration of hydrocarbon. The analysis of biomarkers showed that hydrocarbon come from source rocks deeper than 4 300m.
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As a typical example of lakefacies carbonaterock oil and gas pools consisted by shallow oil pools and mediumdeep gas condensate pools, Nanyishan oil and gas field in the Qaidam Basin has altogether four sets of hydrocarbon source rocks. The whole stratigraphic profile is dominated by argillite, micritic carbonate rock comes second. The reservoirs of hydrocarbon are carbonate rocks, including argillaceous micritic dolostone, argillaceous micritic limestone, micritic limestone, algal limestone, etc. The storage spaces are mainly intercrystal pores, intergranular pores, solution openings, fissures and karst caves. The reservoirs, which have the thickness of 25m in general, have rather stable plane distribution. Tectonic fractures are all welldeveloped from surface to underground. The clear reducing of seismicwave velocity and abnormal highpressure are observed in the mediumdeep layers of hydrocarbondistributive areas. The fissiontrack testing of fractureinfilling calcite revealed that fractures occurred before the generation and migration of hydrocarbon. The analysis of biomarkers showed that hydrocarbon come from source rocks deeper than 4 300m.
Key concepts: Geology, Carbonate, Facies, Dolostone, Karst, Carbonate rock, Geochemistry, Source rock