Lithologic Reservoirs ›› 2026, Vol. 38 ›› Issue (2): 97-110.doi: 10.12108/yxyqc.20260209

• PETROLEUM EXPLORATION • Previous Articles     Next Articles

Heterogeneity and oil control effects of Triassic Chang 7 shale in Zhidan area, Ordos Basin

GUO Yuxin1,2(), BAI Yubin1,2(), ZHAO Jingzhou1,2, ZHANG Jun1,2, CAO Dandan3   

  1. 1 School of Earth Sciences and Engineering, Xi’an Shiyou University, Xi’an 710065, China
    2 Shaanxi Provincial Key Laboratory of Petroleum Accumulation Geology, Xi’an 710065, China
    3 Production Construction HeadquartersYanchang Oilfield Co., Ltd., Yan’an 716000, Shaanxi, China
  • Received:2025-08-26 Revised:2025-09-29 Online:2026-03-01 Published:2026-01-15

Abstract:

The shale oil resource potential of continental petroliferous basins in China is significant,and heterogeneity of the mud shale reservoir controls its oil-bearing and fracability. Based on testings, such as core observation, total organic carbon (TOC) and pyrolysis, whole rock and clay mineral X-ray diffraction analysis, high-pressure mercury intrusion and nitrogen (N2) adsorption experiment, heterogeneity characteristics of Triassic Chang 7 shale reservoir in Zhidan area of Ordos Basin were systematically revealed, and its control effect on shale oil enrichment was discussed. The results show that: (1) Triassic Chang 7 in Zhidan area of Ordos Basin is mainly composed of dark mudstone and black shale, which can be divided into felsic mudstone facies, clayey mudstone facies, and mixed shale facies. The macroscopic heterogeneity of different lithofacies is mainly influenced by terrestrial input,volcanic activity frequency, and sedimentary environments, manifested as the greater frequency of bedding distribution and more frequent changes in lithology, and stronger heterogeneity. On a microscopic level, from clayed mudstone, felsic mudstone to mixed shale, the heterogeneity gradually increases with the increasing frequency of bedding. (2) The mineral composition and TOC content of different lithologies vary significantly, exhibiting strong heterogeneity characteristics. (3) The pore types of Chang 7 mud shale re-servoir in the study area are diverse, including intergranular pores, intragranular pores, clay mineral intercrystalline pores, pyrite intercrystalline pores, and microfractures. The pore structure is mainly mesoporous, with pore diameters ranging from 10 to 100 nm, developing “ink bottle” shaped pores and parallel plate-shaped pores. (4) Lithology, mineral content, TOC content, and pore structure all have controlling effects on Chang 7 shale oil in the study area. Among them, lithofacies, TOC content and average pore diameter have relatively obvious positive correlations with oil-bearing property indicators, which are the main controlling factors for shale oil enrichment. The “sweet spot” segment of shale oil enrichment can be predicted by integrating the heterogeneity characteristics of mud shale, oil-bearing property, brittleness index and movable oil evaluation criteria.

Key words: mud shale, heterogeneity, oil control effect, TOC, shale lithofacies, “sweet spot” evaluation, Chang 7, Triassic, Zhidan area, Ordos Basin

CLC Number: 

  • TE122.2

Fig. 1

Distribution characteristics of shale thickness of Triassic Chang 73 in Zhidan area (a) and comprehensive stratigraphic column of Triassic Chang 7 mud shale (b), Ordos Basin"

Fig. 2

Logging division chart for the mud shale of Triassic Chang 7 in Zhidan area, Ordos Basin"

Fig. 3

Typical lithology and assemblage characteristics of the mud shale of Triassic Chang 7 in Zhidan area, Ordos Basin"

Fig. 4

Well-tie profile of the mud shale of Triassic Chang 7 in Zhidian area, Ordos Basin"

Fig. 5

Microscopic photos of mud shale lithofacies samples with typical heterogeneity characteristic of Triassic Chang 7 in Zhidan area, Ordos Basin"

Fig. 6

Vertical heterogeneity of Triassic Chang 7 mud shale minerals in Zhidan area, Ordos Basin"

Table 1

Statistics of clay mineral types and content of the mud shale of Triassic Chang 7 in Zhidan area, Ordos Basin"

岩相
类型
样品
编号
w(伊利石)/% w(高岭石)/% w(绿泥石)/% w(伊蒙混层)/%
长英
质泥岩
Z4 26.0 1.0 0 73.0
Z29 45.0 10.0 33.0 12.0
Z34 10.0 41.0 26.0 23.0
Z28 65.0 1.0 23.0 11.0
黏土
质泥岩
Z10 62.0 1.0 3.0 34.0
Z11 25.0 10.0 10.0 55.0
Z56 47.0 6.0 25.0 22.0
Z59 77.0 0 13.0 10.0
混合
质页岩
Z31 34.0 17.0 25.0 24.0
Z33 56.0 9.0 21.0 14.0
Z35 18.0 25.0 27.0 30.0
Z1 9.0 7.0 28.0 56.0
Z2 17.0 4.0 13.0 66.0
Z3 14.0 4.0 12.0 70.0
Z5 8.0 6.0 15.0 71.0
Z7 11.0 13.0 20.0 56.0

Fig. 7

Microscopic characteristics of scanning electron microscopy of the mud shale of Triassic Chang 7 oil-layer group in well S380 in Zhidan area, Ordos Basin"

Fig. 8

N2 adsorption-desorption, capillary pressure curves and pore diameter distribution of Triassic Chang 7 oil-layer group in Zhidan area, Ordos Basin"

Fig. 9

Distribution characteristics of free hydrocarbon content (S1) and chloroform asphalt “A” content of different lithofacies of Triassic Chang 7 oil-layer group in Zhidan area, Ordos Basin"

Fig. 10

Correlation of pyrolysis free hydrocarbons and chloroform asphalt “A” content with inorganic mineral content of Triassic Chang 7 oil-layer group in Zhidan area, Ordos Basin"

Fig. 11

Correlation of pyrolysis free hydrocarbon, chloroform asphalt “A” and its group components with TOC of different lithology mudstones of Triassic Chang 7 oil-layer group in Zhidan area, Ordos Basin"

Fig. 12

Correlation of TOC content, S1 and chloroform asphalt ‘A’ content with average pore diameter of Triassic Chang 7 oil-layer group in Zhidan area, Ordos Basin"

Table 2

Evaluation criteria for shale oil “sweet spot” of Triassic Chang 7 oil-layer group in Zhidan area,Ordos Basin"

“甜点”
等级
可压性 含油性 可动性
脆性
指数/%
非均质性结果(级差) S1/
(mg·g-1
非均质性结果(级差) OSI/
(mg·g-1·
TOC -1
非均质性结果
(级差)
有利靶点类(一类) ≥ 60 1.44 ≥ 5 1.19 > 100 1.73
潜在资源类(二类) 40~60 1.34 3~5 1.13 > 70 1.76
补充资源类(三类) 40~60 1.27 3~5 1.09 < 70 1.18

Fig. 13

Comprehensive analysis of Triassic Chang 7 oil-layer group of well G135 in Zhidan area, Ordos Basin"

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