Special Oil & Gas Reservoirs ›› 2024, Vol. 31 ›› Issue (3): 18-26.DOI: 10.3969/j.issn.1006-6535.2024.03.003

• Geologic Exploration • Previous Articles     Next Articles

Characterization of Tight Sandstone Reservoirs and Prediction of Favorable Reservoirs in the Fourth Member of the Upper Triassic Xujiahe Formation in the Tianfu Area of the Sichuan Basin

Qiu Yuchao1,2,3, Xu Qiang1,2, Li Yibo1,2, Deng Wei1,2, Zheng Chao3, Zhao Zhengwang3, Jin Zhimin3, Tan Xiucheng1,2*   

  1. 1. Sichuan Province key Laboratory of Natural Gas Geology, Southwest Petroleum University, Chengdu, Sichuan 610500, China;
    2. Southwest Petroleum University, Chengdu, Sichuan 610500, China;
    3. PetroChina Southwest Oil and Gas Field Company, Chengdu, Sichuan 610041, China
  • Received:2023-07-03 Revised:2024-03-28 Online:2024-06-25 Published:2024-07-26

Abstract: The fourth member of the Upper Triassic Xujiahe Formation in the Tianfu Area of the Sichuan Basin (referred to as the T3x4) is characterized by thick sandstone layers interbedded with thin mudstone layers,making it a crucial exploration target for tight sandstone gas reservoirs.However,due to limitations in seismic vertical resolution,thin mudstone layers are hard to be determined by conventional methods,hindering the precise characterization of sandstone in this interval.This limitation has impeded the understanding of the distribution patterns of sand bodies in the basin and identification of favorable target areas.To address these issues, this study integrates drilling data with seismic facies and establishes a mapping relationship between the two.Under the constraint of natural gamma-ray curves,optimal inversion frequency parameters were sought to enhance the accuracy of inter-well sand body prediction.The distribution characteristics of the T3x4 sandstone in the Upper Triassic Xujiahe Formation were well characterized with waveform indication simulation method.The results indicate that the T3x4 sandstone exhibits characteristics of being thick in the west (55.0 to 100.0 m) and thin in the east (15.0 to 50.0 m).Compared to the third member of the Xujiahe Formation,the transition zone of sand body thickness variation (slope break zone) has migrated towards the interior of the craton.Analyzing data from 18 wells within the seismic working area,it was observed that beneath the slope break zone,the sandstone has a high average porosity (8.0%) and a large reservoir thickness (45.4 m).Considering tectonic evolution, sedimentary facies distribution,sandstone thickness,and porosity variations,it is proposed that the T3x4 follows a pattern of structures control slope break zones,and slope break zones control reservoirs.Regions below the slope break zones exhibit favorable reservoir properties with good physical characteristics and significant thickness,making them promising exploration areas.The study results provide valuable insights for the in-depth exploration of the T3x4.

Key words: thick Sandstone, Sandstone characterization, waveform indication simulation, well-seismic integration, reservoir prediction, Xujiahe Formation, Sichuan Basin

CLC Number: