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- W2361900545 abstract "The Jurassic-Cretaceous reservoirs in Block Ⅲ in the central Junggar basin are deep and high-quality reservoirs with burial depth ranging from 5800 to 6100 m and relatively good poroperm characteristics. In order to reveal their mechanisms of formation, various methods, including observation of cast thin section, division of diagenetic sequences, analysis of energy field and basin modeling, are used to study these reservoirs in depth based on a thorough study of the characteristics of the Jurassic-Cretaceous reservoirs in the study area. The following understandings are obtained. ① Sandbodies with relatively strong hydrodynamic conditions were the basis for the formation of deep reservoirs; ② The existence of low geothermal field might effectively impede diagenesis, resulting in the preservation of the primary pores; ③ Late rapid burial resulted in uncompaction of the formations and anomalous pressure, thus the reservoirs still preserved relatively good poroperm characteristics in deep burial; ④ Early fresh water dissolution and late organic acid dissolution greatly improved the poroperm characteristics of the reservoirs; ⑤ Appropriate amount of rim chlorite also played an active role in the protection of reservoirs. The combined actions of the above factors led to the development of high-quality reservoirs with very large burial depth." @default.
- W2361900545 created "2016-06-24" @default.
- W2361900545 creator A5040850104 @default.
- W2361900545 date "2008-01-01" @default.
- W2361900545 modified "2023-09-22" @default.
- W2361900545 title "FORMATION MECHANISM OF HIGH QUALITY JURASSIC-CRETACEOUS RESERVOIRS IN THE CENTRAL JUNGGAR BASIN" @default.
- W2361900545 hasPublicationYear "2008" @default.
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