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Huang Jixiang, Zeng Wei, Zhang Gaoxing, Ran Hong. The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin[J]. Acta Sedimentologica Sinica, 1995, 13(S1): 109-117.
Citation: Huang Jixiang, Zeng Wei, Zhang Gaoxing, Ran Hong. The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin[J]. Acta Sedimentologica Sinica, 1995, 13(S1): 109-117.

The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin

  • Received Date: 1994-05-10
  • Publish Date: 1995-12-10
  • The 2-section of Jialingjang Group of Triassic in the eastern part of Sichuan Basin is an important gas bearing position. The Development of bank-micro factes have played an important pole in controlling the gas pool of fracture-pore type in traps.The banks are POint-bank on the platform in upper yangtze epicontinental sea. The new classificantion of shallow-sea bank and shallow exposed banks has been suggested on the basis of the evolution model of depositional environments which were controlled by relative sea-level changes. The similarities and difference of two types of banks have been compared. There were four bank development periods in the multicycle sedements of 2-section of Jialingjiang Group.The distribution of banks in two bank-development periods, for example, the 2-subsection of 2-section, have been mapped. The composition and devolopment model of point-bank at the Tishan anticline has been analysed. It clearly points out that the lithic factes in the core of bank have big thickness and good continuity in the multi-bank development periods. There are three types of factes sequences models:(1) the banks developed with sea-level up and disappeared with sea-level down; (2) the banks developed with sea-level down and disappeared to expose ; and (3) the banks developed with sea-level up and disappeared with sea-level up.Finally, the authors state how the shallow exposed bank control the formation of gas-pool. It has been recognind: ①the bank-microfacies complexs are beneficial for complexs of oil-producing, reservoir and seal formations, ②the shallow exposed bank is the microfacies zone of the pore-layers devolopment, ③ the sediment-diagenetic trap formed in bank-microfacies zone is beneficial for early accumulation of oil and gas pools @the development of pore-layers and accumulation of oil and gas in early sediment-diagenetic traps are the base of present gas -pool of fracture-pore type in various traps.
  • [1] 1.l曾允孚、夏文杰主编,1986,沉积岩石学,北京:地质出版社。

    2. Scholle , P. A.,Bebout, D. G.,and Moore, C. H.,1983, eds, Carbonate Depositional Environments, A. A. P. G.Memoir 33.

    3.王英华主编,1991,中下扬子地区海相碳酸盐岩成岩作用研究,北京:科学技术出版社。

    4.方少仙、黄继祥等,1989,中国南方泥盆、石炭纪岩相古地理及含油气性研究,《沉积相研究文集》编委会主编,《含油气盆地沉积相与油气分布》,北京:石油工业出版社。
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  • Received:  1994-05-10
  • Published:  1995-12-10

The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin

Abstract: The 2-section of Jialingjang Group of Triassic in the eastern part of Sichuan Basin is an important gas bearing position. The Development of bank-micro factes have played an important pole in controlling the gas pool of fracture-pore type in traps.The banks are POint-bank on the platform in upper yangtze epicontinental sea. The new classificantion of shallow-sea bank and shallow exposed banks has been suggested on the basis of the evolution model of depositional environments which were controlled by relative sea-level changes. The similarities and difference of two types of banks have been compared. There were four bank development periods in the multicycle sedements of 2-section of Jialingjiang Group.The distribution of banks in two bank-development periods, for example, the 2-subsection of 2-section, have been mapped. The composition and devolopment model of point-bank at the Tishan anticline has been analysed. It clearly points out that the lithic factes in the core of bank have big thickness and good continuity in the multi-bank development periods. There are three types of factes sequences models:(1) the banks developed with sea-level up and disappeared with sea-level down; (2) the banks developed with sea-level down and disappeared to expose ; and (3) the banks developed with sea-level up and disappeared with sea-level up.Finally, the authors state how the shallow exposed bank control the formation of gas-pool. It has been recognind: ①the bank-microfacies complexs are beneficial for complexs of oil-producing, reservoir and seal formations, ②the shallow exposed bank is the microfacies zone of the pore-layers devolopment, ③ the sediment-diagenetic trap formed in bank-microfacies zone is beneficial for early accumulation of oil and gas pools @the development of pore-layers and accumulation of oil and gas in early sediment-diagenetic traps are the base of present gas -pool of fracture-pore type in various traps.

Huang Jixiang, Zeng Wei, Zhang Gaoxing, Ran Hong. The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin[J]. Acta Sedimentologica Sinica, 1995, 13(S1): 109-117.
Citation: Huang Jixiang, Zeng Wei, Zhang Gaoxing, Ran Hong. The Development and Distribtuion of the Triassic Bank-Microfacies in the 2-Section of Jialingjiang Group and Its Gas-Poal Control Nature in the Eastern Part of Sichuan Basin[J]. Acta Sedimentologica Sinica, 1995, 13(S1): 109-117.
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