Lithologic Reservoirs ›› 2025, Vol. 37 ›› Issue (2): 81-91.doi: 10.12108/yxyqc.20250208

• PETROLEUM EXPLORATION • Previous Articles    

Sedimentary evolution and favorable reservoir distribution of Permian Qixia Formation in the southern margin of Deyang-Mianyang Sag, Sichuan Basin

LI Ya1, WANG Wei1, ZHAO Like1, LIU Ran1, ZHANG Xihua1, CHEN Yangui1, HUANG Tianhai2, XIAO Di2   

  1. 1. Research Institute of Exploration and Development, PetroChina Southwest Oil and Gas Field Company, Chengdu 610041, China;
    2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu 610500, China
  • Received:2024-04-19 Revised:2024-11-26 Published:2025-03-06

Abstract: Based on the comprehensive analysis of core samples,cuttings,well logging,and seismic data,this study investigates the sedimentary microfacies characteristics and evolutionary processes of the Permian Qixia Formation in the southern margin of the Deyang-Mianyang depression,Sichuan Basin. Furthermore,the research delineates favorable reservoir zones based on the aforementioned analysis. The results show that:(1)The southern margin of the Deyang-Mianyang depression in the middle Permian Qixia period is a set of carbonate ramp facies deposits,which are further subdivided into shallow Gentle Slope,deep Gentle Slope-basin subfacies and a variety of microfacies. The lithology is dominated by grained dolomite,sparry bioclastic limestone,micrite bioclastic limestone,bioclastic micrite limestone,micrite limestone and argillaceous limestone.(2)During the sedimentary period of Qi1 Member,the water is relatively deep and the overall development of the beach facies was low. It was only deposited in the Gaoshitai area with relatively high paleotopography. The lithology was dominated by micritic bioclastic limestone,and the sedimentary facies was greatly influenced by the paleotopography. During the lower of Qi2 sedimentary period,the water became shallower,and the shoal facies developed in Gaoshiti area in the upper part of the paleogeomorphology migrated laterally to Moxi area in the lower part of the paleogeomorphology due to the lack of space to accommodate it,the difference of sedimentary geomorphology decreased and reverse. During the upper of Qi2 sedimentary period,the shoal facies in the Moxi area not only experienced vertical accretion but also progressively migrated and expanded towards the Penglai region. Although the topographic relief of the depositional environment decreased during this phase,no significant inversion occurred.(3)The Qixia Formation is mainly composed of dolomite reservoirs,and its development is mainly controlled by factors such as lithology,karst,and fractures. The relatively high-energy particle beach, due to its relatively high sedimentary topography,is prone to exposure and early karstification,forming highquality reservoirs. The high porosity and permeability provide fluid channels for further stacking of dolomite. The high-energy beach is the most developed in the Moxi area,which is the most favorable reservoir zone in the study area,followed by the Penglai area in the north. The periphery of the“Deyang-Mianyang”depression is expected to become the next natural gas accumulation area with a certain scale of facies control.

Key words: particle beach, sedimentary paleogeomorphology, carbonate gentle slope, early karstification, dolo-mitization, Qixia Formation, Permian, Deyang-Mianyang depression, Sichuan Basin

CLC Number: 

  • TE122
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