Citation: | Cai-yuan Dong, Liang Zhang, Wei Yang, Zhen-ping Xu, Jun Li, Wei-dong Miao, 2025. Accumulation process and potential of Jurassic tight sandstone oil and gas in Eastern Yangxia sag of Kuqa Depression, China Geology, 8, 389-407. doi: 10.31035/cg2023063 |
The Jurassic tight sandstone oil and gas exploration and development in the eastern Yangxia Sag is a new field. To elucidate the origin, accumulation process and potential of tight oil and gas, the authors have conducted comprehensive analyses employing methodologies encompassing source rocks, oil geochemistry, and fluid inclusions. The results show that the abundance of organic matter of Jurassic source rocks is high, and the type of organic matter is of II-III and in mature evolution stage. The main source rocks of oil and gas are Huangshanjie Formation and Jurassic coal-bearing source rocks. Ahe Formation developed two stages of hydrocarbon charging, and the period is later than the reservoir densification time. Yangxia Formation oil charged before the reservoir densified, and the late gas charged after the reservoir densified. Hydrocarbon generation intensity of Jurassic source rocks has reached the basic conditions for the formation of tight gas reservoirs. Controlled by the difference of source rocks distribution and accumulation process, tight sandstone oil and gas accumulation conditions are better in the depression direction than in the southeast margin area. This study is of practical importance for expanding the exploration field and selecting favorable areas in the eastern Yangxia sag.
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Position of the research region and stratigraphic composite histogram in Kuqa Depression (modified from Liu JL et al., 2016; Wan JL et al. 2022).
Core samples from Yangxia Formation and Ahe Formation in Yangxia sag.
Relationship between TOC and (S1+S2) of Triassic-Jurassic source rocks in Yangxia sag.
Kerogen type identification of source rocks with different strata and different lithologies in Yangxia sag.
Characteristics of terpanes (m/z=191) and steranes (m/z=217) in Triassic and Jurassic source rocks. Note: C24Tet, C24 tetracyclic terpanes; C26 TT, C26 tetracyclic terpanes; C30H, C30 hopanes; D, C30 rearranged hopanes; G, gammacerane. a, b‒Mudstone, Triassic Huangshanjie Formation; c, d‒mudstone, Jurassic Qiakemake Formation; e‒Carbonaceous mudstone, Jurassic Yangxia Formation; f‒mudstone, Jurassic Kezilenur Formation; g‒mudstone, Triassic Taliqike Formation.
Distribution characteristics of biomarker in crude oil of Yangxia Formation (a) and Ahe Formation (b) in Yangxia sag. Note: C24Tet, C24 tetracyclic terpanes; C26 TT, C26 tetracyclic terpanes; C30H, C30 hopanes; D, C30 rearranged hopanes; G, gammacerane.
Rock classification of sandstone reservoirs of Yangxia and Ahe Formations in Yangxia sag (a) and their porosity and permeability comparison (b and c). Ⅰ‒Quartz sandstone; Ⅱ‒feldspar quartz sandstone; Ⅲ‒lithic quartz sandstone; Ⅳ‒feldspar sandstone; Ⅴ‒lithic feldspar sandstone; Ⅵ‒feldspar lithic sandstone; Ⅶ‒lithic sandstone.
Pore types of sandstone reservoirs of Jurassic Ahe Formation and Yangxia Formation in Yangxia sag. a‒Well YT-1, 7787.64 m, J1a, lithic sandstone. There are intergranular dissolved pores in the rock, and feldspar dissolution is relatively common, leading to the formation of intra - granular dissolved pores. There is less debris. The rock cracks are highly developed, cutting through particles intermittently, extending in parallel, and connecting with the pores. b‒Well YT-1, 7791.60 m, J1a, lithic sandstone. The pores are mainly grain - dissolved pores. Feldspar dissolution is more obvious, and dissolution occurs along the cleavage and cracks, forming sieve - like dissolved pores. Debris dissolution is less. Microcracks are parallel to the plane and are distributed intermittently. c‒Well YX-2, 5295.87 m, J1y, coarse-grained feldspar lithic sandstone. There are only a few intra - granular dissolution pores. Micro - cracks can be seen in feldspar and some lithic grains at the edges of a few particles. d‒Well YX-2, 5304.90 m, J1y. There are a small number of intergranular pores in coarse-grained lithic sandstone, solution pores in feldspar, micropores in argillaceous material, and a small number of grain margin fractures and microfractures extending through the particles.
Diagenetic characteristics of tight reservoirs in Ahe and Yangxia formations in Yangxia sag.
Fitting curve of porosity and surface porosity.
Characteristics of dynamic accumulation process in Well YT-1.
Photomicrographs of representative inclusions under transmitted and UV light observed. (a), (b) and (c), inclusion characteristics of Ahe Formation in Well YT-1; a‒oil inclusions with yellow fluorescence colour; b‒oil inclusions with blue-white fluorescence colour; c‒gaseous inclusion, no fluorescence. (d), (e) and (f), inclusion characteristics of Yangxia Formation in Well YX-2; d‒oil inclusions with yellow fluorescence colour; e‒oil inclusions with blue-white fluorescence colour; f‒gaseous inclusion, no fluorescence.
Characteristics of dynamic accumulation process in Well YX-2.
Plane distribution of gas intensity of Jurassic source rocks in Eastern Yangxia Sag.