Lithologic Reservoirs ›› 2026, Vol. 38 ›› Issue (4): 137-147.doi: 10.12108/yxyqc.20260412

• PETROLEUM EXPLORATION • Previous Articles     Next Articles

Restoration and geological implications of paleogeomorphology during the depositional period of Triassic Feixianguan Formation in Puguang area, northeastern Sichuan Basin

YANG Weiqiang1,2(), LI Zhongchao3, ZHANG Jixi1, WANG Yi1, ZHAO Zhen1   

  1. 1 Exploration and Development Research Institute, Zhongyuan Oilfield Company, Sinopec, Puyang 457001, Henan, China
    2 Key Laboratory of High Acid Gas Field Development, Sinopec, Puyang 457001, Henan, China
    3 Zhongyuan Oilfield Company, Sinopec, Puyang 457001, Henan, China
  • Received:2025-12-11 Revised:2026-01-20 Online:2026-07-01 Published:2026-07-06

Abstract:

Paleogeomorphologic framework exerts significant control on the spatial distribution of facies-controlled carbonate reservoirs. Based on geophysical data such as core thin sections, conventional logging data, the original thickness of individual wells in Triassic Feixianguan Formation was restored in Puguang area through analysis of differential compaction and pressure dissolution of lithofacies. Combined with 3D seismic data, the paleogeomorphology was reconstructed, and the structural subsidence of individual wells was identified using the INPEFA curve. The decompaction and pressure dissolution restoration results were integrated to further refine the paleogeomorphology during the depositional period. Research results show that: (1) Feixianguan Formation in Puguang area develop seven major rock types, including granular dolomite, micritic-granular dolomite, crystalline dolomite, micritic dolomite, granular limestone, micritic-granular limestone, and micritic limestone. Based on compaction recovery coefficients and pressure dissolution recovery coefficients, decompaction coefficients of different lithofacies were calculated. Granular dolomite exhibits the smallest decompaction coef-ficient of 1.25, indicating little change between its present-day thickness and original sedimentary thickness, whereas micritic limestone exhibits a relatively large decompaction coefficient of 3.09, with its present-day thickness differing by more than two times from the original thickness. (2) The identification of tectonic subsidence using the INPEFA method is a single-well sequence identification technique based on GR curve trend spectrum analysis. Combined with Walther’s law, the key mechanism of this method for identifying tectonic subsidence was clarified, and the INPEFA mean value of 0.5 was used as the threshold to distinguish normal sedimentary areas and tectonic subsidence areas. (3) The distribution of shoal deposits is controlled by paleogeomorphology and tectonic subsidence. In tectonic stable areas, shoal deposits are concentrated in high parts of the paleogeomorphology; whereas in tectonic active areas, shoal deposits develop in regions with positive paleogeomorphology and the INPEFA mean value of less than 0.5. (4) The accuracy of paleogeomorphology restored through decompaction, pressure dissolution, and tectonic subsidence analysis has been significantly improved, which can effectively identify and eliminate spurious topographic highs caused by differential subsidence, thus more clearly revealing controlling effects of paleogeomorphology on the development of high-quality reservoirs.

Key words: paleogeomorphology reconstruction, decompaction and pressure dissolution, INPEFA curve, tectonic subsidence, shoal facies, Feixianguan Formation, Triassic, Puguang area, northeastern Sichuan Basin

CLC Number: 

  • TE122

Fig. 1

Planar distribution of sedimentary facies (a) and comprehensive stratigraphic column of Triassic Feixianguan Formation (b) in Puguang area, northeastern Sichuan Basin"

Fig. 2

Microphotos of thin section from Triassic Feixianguan Formation in Puguang area, northeastern Sichuan Basin"

Fig. 3

Parameter model for decompaction and pressure solution of carbonate rock stratigraphic thickness of Triassic Feixianguan Formation in Puguang area, northeastern Sichuan Basin"

Table 1

Decompression coefficients of different lithofacies of Triassic Feixianguan Formation in Puguang area, northeastern Sichuan Basin"

岩性 压实恢复系数 压溶恢复系数 解压系数
颗粒灰岩 1.2 1.090 1.31
泥晶颗粒灰岩 1.5 1.127 1.69
泥晶灰岩 2.5 1.236 3.09
颗粒白云岩 1.2 1.038 1.25
泥晶颗粒白云岩 1.5 1.053 1.58
泥晶白云岩 2.5 1.084 2.71

Fig. 4

Stratigraphic thickness of paleogeomorphy before and after restoration of Member 1-2 of Triassic Feixianguan Formation in Puguang area, northeastern Sichuan Basin"

Fig. 5

INPEFA curves of Member 1-2 of Triassic Feixianguan Formation in well Maoba 4, Puguang area, northeastern Sichuan Basin"

Fig. 6

Well-tie correlation of INPEFA curves of Member 1-2 of Triassic Feixianguan Formation across well Yangliu 1-well Puguang 8-well Puguang 5 in Puguang area, northeastern Sichuan Basin"

Fig. 7

Scatter plot of INPEFA curve mean values and paleogeomorphology of Member 1-2 of Triassic Feixianguan Formation in Puguang area, northeastern Sichuan Basin"

Fig. 8

Scatter plot of grain beach thickness and paleogeomorphology before (a) and after (b) restoration of paleo-geomorphology of Member 1-2 of Triassic Feixianguan Formation in Puguang area, northeastern Sichuan Basin"

Fig. 9

Comparison of paleogeomorphology before and after decompaction and pressure dissolution restoration of stratigraphic thickness of the second sequence of Member 1-2 of Triassic Feixianguan Formation in Maoba-Dawan area, northeastern Sichuan Basin"

Fig. 10

Paleogeomorphology after decompaction and pressure dissolution restoration of stratigraphic thickness and INPEFA mean values of the second sequence of Member 1-2 of Triassic Feixianguan Formation in Maoba-Dawan area, northeastern Sichuan Basin"

Fig. 11

Gas reservoir profiles of Triassic Feixianguan Formation across well Fen 3-well Maoba 1-well Dawan 102-well Puguang 6-well Puguang 12 in tectonic active zones of Puguang area, northeastern Sichuan Basin"

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