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- W2381796727 abstract "Ordovician carbonate rocks in Tazhong area,Tarim Basin have a complicate burial and thermal history.They were experienced multistage tectogenesis and reconstructed by deep fluids,so their diagenesis was complicated.According to rock-mineral identification,fluid inclusion petrography,homogenisation temperature and salinity measurement of Ordovician carbonate rock samples of 6 well,and combining with tectonic evolutional,burial and thermal history data,diagenesis and deep hydrothermal fluids of Ordovician carbonate rocks from the Tazhong area are researched in this paper.Fluid inclusions of Ordovician carbonate rocks can be divided into four groups.The first group was formed at contemporaneous-penecontemporaneous or epidiagenetic stage of early diagenesis period from late Caledonian to early Hercynian,its homogenization temperature is less than 50~60 ℃.The second group was formed at shallow burial diagenesis period of late Hercynian,its homogenization temperature is in the range from 90 ℃ to 105 ℃.The third group was formed at the period from wave burial to deep burial diagenesis,its homogenization temperature is in the range from 90 ℃ to 105 ℃.The homogenization temperature of the forth group is higher and concentrates in the range from 192 ℃ to 235 ℃.The formation of the forth group of high temperature fluid inclusions is most likely related with magmatism or deep hydrothermal fluids.Besides,the phenomenon that salinity varies with the increase of homogenization temperature shows that the Ordovician carbonate rocks in Tazhong area were influenced by deep hydrothermal fluids." @default.
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- W2381796727 date "2011-01-01" @default.
- W2381796727 modified "2023-09-28" @default.
- W2381796727 title "Ordovician Carbonate Rock Inclusion Features and Its Indicative Significance to Diagenesis and Deep Fluids Action in Tazhong Area,Tarim Basin" @default.
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