Lithologic Reservoirs ›› 2026, Vol. 38 ›› Issue (2): 134-144.doi: 10.12108/yxyqc.20260212

• PETROLEUM EXPLORATION • Previous Articles     Next Articles

Characteristics and oil-source correlation of Triassic Chang 7 member source rocks in Huanxian area, Ordos Basin

LI Tao1(), MA Guofu2, ZHAO Leyi2(), YUAN Li2, MA Qilin2, XIE Jingyu2, ZHANG Bo2, LI Henan2   

  1. 1 Department of Exploration, PetroChina Yumen Oilfield Company, Jiuquan 735019, Gansu, China
    2 Research Institute of Exploration and Development, PetroChina Yumen Oilfield Company, Jiuquan 735019, Gansu, China
  • Received:2025-07-11 Revised:2025-09-23 Published:2026-01-20 Online:2026-03-01

Abstract:

Triassic Chang 7 member shale is the main source rock in Huanxian area of the western Ordos Basin. Through rock pyrolysis, total organic carbon measurement, gas chromatography-mass spectrometry, and AI-assisted comprehensive biomarker analysis, geochemical characteristics of crude oils and source rocks were systematically studied,the origin of crude oil and the proportion of hydrocarbon supply from mudstones and shales were clarified, and their hydrocarbon accumulation models were explored. The results show that: (1) Triassic Chang 7 member in the eastern Huanxian area is primarily developed shale,characterized by high organic matter abundance, favorable organic matter type, significant hydrocarbon generation potential. In contrast, the western part is dominated by dark mudstone, with TOC values ranging from 0.40% to 6.23%, hydrocarbon generation potential (S1 + S2) of 0.50-13.13 mg/g, organic matter types of TypeⅡ and Ⅲ, and an average vitrinite reflectance (Ro) of 0.84%, indicating a mature stage. It belongs to a medium-poor source rock with relatively lower hydrocarbon generation potential compared to shale. (2) Biomarker compositions of eastern shales and western mudstones are fundamentally similar, but significant differences exist in certain biomarker parameter ratios. Eastern shales exhibit low Pr/Ph ratios, high Ts/Tm, C29Ts/C29H, C30*/C29H, and C30*/C30H values. In contrast, western dark mudstones display relatively high Pr/Ph ratios, low Ts/Tm, C29Ts/C29H, C30*/C29H, and C30*/C30H values. These differences reflect the controlling effect of paleo-sedimentary environments on the development of mudstones and shales in the study area. (3) Chang 8 member in the study area develops three types of crude oil: Type A is crude oil predominantly from the eastern Chang 8 member, exhibiting high Ts/Tm and C29Ts/C29H values, along with relative high C30*/C29H and C30*/C30H values, type A is primarily derived from eastern shales. Type C, though currently less abundant, is characterized by low Ts/Tm, C29Ts/C29H, C30*/C29H, and C30*/C30H values, predominant sourcing from western mudstone. Type B, found in the western Chang 8 member, displays intermediate biomarker between type A and type C, with moderate Ts/Tm, C29Ts/C29H, C30*/C29H, and C30*/C30H values. It is a mixed crude oil composition dominantly contributed by eastern shales.

Key words: shale, geochemical characteristics, biomarkers, oil-source correlation, the 7th member of Yanchang Formation, Triassic, Huanxian area, Ordos Basin

CLC Number: 

  • TE122.2

Fig. 1

Structural location of Huanxian area (a) and stratigraphic column of Triassic Chang 7 member (b), Ordos Basin"

Fig. 2

Box plot of geochemical element ratios of Triassic Chang 7 member in Huanxian area, Ordos Basin"

Fig. 3

Core photographs of shale and mudstone of Triassic Chang 7 member in Huanxian area, Ordos Basin"

Fig. 4

Thickness distribution of Triassic Chang 7 source rocks in Huanxian area, Ordos Basin"

Fig. 5

Hydrocarbon generation potential and organic matter abundance of Triassic Chang 7 source rocks in Huanxian area, Ordos Basin"

Fig. 6

Crossplot of Ph/nC17-Pr/nC18 of Triassic Chang 7 shales and dark mudstones in Huanxian area, Ordos Basin"

Fig. 7

Biomarker chromatograms of Triassic Chang 7 source rocks in Huanxian area, Ordos Basin"

Fig. 8

Biomarker chromatograms of Triassic Chang 8 crude oil in Huanxian area, Ordos Basin"

Fig. 9

Comparison of biomarker parameters of Triassic Chang 8 crude oil and Chang 7 source rock in Huanxian area, Ordos Basin"

Table 1

Statistics of depositional environment indices of Triassic Chang 7 source rocks and crude oils in Huanxian area, Ordos Basin"

样品类型 区域 井号 层位 沉积环境指数(DEI)
烃源岩 页岩 东部 H102 长73 0.085
泥岩 长72 0.120
泥岩 西部 H804 长73 0.065
H82 长72 0.033
原油 东部 H12 长8 0.083
西部 H92 长8 0.079
H94 长8 0.072

Fig. 10

Hydrocarbon accumulation models of Triassic Chang 81 in Huanxian area, Ordos Basin"

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