摘要
Paleo-pressure reconstruction in sedimentary basins is one of the most important aspects of hydrocarbon accumulation research.In view of the advantages and disadvantages of the current methods for paleo-pressure research,a new method to reconstruct the paleo-pressure is presented in this paper.According to the geological background,quantitative analyses of the factors that might control overpressure were first conducted to clarify the contributions of each mechanism during different geological periods.Pressure evolution was reconstructed by fluid-compaction modelling with constraints imposed by the paleo-pressures obtained from fluid inclusions or differential stress methods.Determining the mechanisms responsible for overpressures during geological history is the basic prerequisite for paleo-pressure research.Thus,quantitative studies were conducted of the contributions of disequilibrium compaction,gas charging,oil cracking,temperature reduction,and tectonic uplift and subsidence to overpressures.Three case studies of paleo-pressure reconstruction were performed for the Sinian strata in the Sichuan Basin,Ordovician strata in the north uplift in the Tarim Basin and the Permian strata in the Sulige Gas Field in the Ordos Basin,where these three study sites are normally pressured,weakly over-pressured and abnormally low pressured at present,respectively.The new method developed in this paper is very important for the practical reconstruction of the paleopressure in marine strata and ancient strata in deep basins.
基金
supported by the National Natural Science Foundation of China(Grant Nos.41830424,41125010)
the National Science and Technology Major Project(Grant No.2016ZX05007003005)
Beijing Science and Technology New Star and Leading Talent Training Program(Grant No.Z171100001117163)。
