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- W2390766484 abstract "The main diagenesis of the Yanchang Formation sandstone reservoirs in the Fuxian-Zhengning area,Ordos Basin,includes compaction,cementation,corrosion and fracturation,and diagenetic authigenic minerals in these reservoirs are dominated by chlorite,authigenetic quartz and calcite.Two phases of hydrocarbon inclusions have been identified according to the time sequence of the formation of host diagenetic minerals,the earlier one composed of mostly brine inclusions that contain gaseous or liquid hydrocarbons either occurs along healed microfractures wrapped up by secondary growth edges of quartz or feldspar,or is trapped at the bottom of secondary growth edges of quartz or feldspar,while the later one mostly consisting of gas-liquid or liquid hydrocarbon inclusions occurs along the late-formed microfractures or in sparry calcite cements.Homogenization temperatures measured from brine inclusions associated with hydrocarbon ones show a bimodal distribution in the ranges with 110～120℃ and 140～150℃ as peak temperatures correspondingly,indicating the early and late formation of reservoirs,respectively.Integrated with salinity and density analyses,we suggested a one-stage and two-episode model for the major accumulation of hydrocarbons in the Yanchang Formation of the study area,which is characterized by compacting while charging.Analytical data of fluid inclusions and illitic K-Ar isotope dating,combined with burial history,also showed that the late stage of Early Cretaceous(120～95Ma B.P.) is the major period of hydrocarbon accumulations in the Fuxian-Zhengning area." @default.
- W2390766484 created "2016-06-24" @default.
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- W2390766484 date "2011-01-01" @default.
- W2390766484 modified "2023-09-26" @default.
- W2390766484 title "Classification of hydrocarbon accumulation phases of the Yanchang Formation in the Fuxian-Zhengning area,Ordos Basin" @default.
- W2390766484 hasPublicationYear "2011" @default.
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