2021
DOI: 10.1007/s12583-020-1083-6
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Conglomerate Reservoir Pore Evolution Characteristics and Favorable Area Prediction: A Case Study of the Lower Triassic Baikouquan Formation in the Northwest Margin of the Junggar Basin, China

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Cited by 20 publications
(6 citation statements)
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“…Exploration in the study area began in the 1980 s, and the Fengcheng Formation (P 1 f) of the Marbei slope (Pf) was located in the Xiazijie nosedive zone during both the Jurassic and Cretaceous orogenic periods, and present-day tectonics suggest that the area is still nosedive at present (Ma et al, 2022;Chen et al, 2022;Shi et al, 2022;Lu et al, 2023). The development of two large-scale retrograde fractures is the main through-origin fracture in this area, and the large-scale fractures are accompanied by microfractures around them (Xiao et al, 2021). Oil test in the well section of 4,831.0-4,886.0 m in the P 1 f 1 layer of the Permian Fengcheng Formation yielded 3.65 t of oil per day from a 4 mm nozzle and 1.48 m 3 of water per day; oil test in the well section of 4,683.0-4,701.0 m in the P 1 f 2 layer of the Permian Fengcheng Formation without fracturing yielded 0.54 t of oil per day from a 4 mm nozzle; oil test in the well section of 4,571.0-4,594.0 m in the P 1 f 3 layer of the Permian Fengcheng Formation, stratigraphic test, obtained 1.13 t of oil per day.…”
Section: Tectonic Location and Geologic Structurementioning
confidence: 99%
“…Exploration in the study area began in the 1980 s, and the Fengcheng Formation (P 1 f) of the Marbei slope (Pf) was located in the Xiazijie nosedive zone during both the Jurassic and Cretaceous orogenic periods, and present-day tectonics suggest that the area is still nosedive at present (Ma et al, 2022;Chen et al, 2022;Shi et al, 2022;Lu et al, 2023). The development of two large-scale retrograde fractures is the main through-origin fracture in this area, and the large-scale fractures are accompanied by microfractures around them (Xiao et al, 2021). Oil test in the well section of 4,831.0-4,886.0 m in the P 1 f 1 layer of the Permian Fengcheng Formation yielded 3.65 t of oil per day from a 4 mm nozzle and 1.48 m 3 of water per day; oil test in the well section of 4,683.0-4,701.0 m in the P 1 f 2 layer of the Permian Fengcheng Formation without fracturing yielded 0.54 t of oil per day from a 4 mm nozzle; oil test in the well section of 4,571.0-4,594.0 m in the P 1 f 3 layer of the Permian Fengcheng Formation, stratigraphic test, obtained 1.13 t of oil per day.…”
Section: Tectonic Location and Geologic Structurementioning
confidence: 99%
“…Among them, conglomerate oil reservoirs have attracted great attention because of their rich geological reserves and large development potential [ 3 , 4 , 5 , 6 ]. However, conglomerate reservoirs are a special kind of lithologic reservoir, and they still present problems worldwide due to their complex and variable lithology, the complex modal characteristics of pores, poor reservoir physical properties, and strong heterogeneity [ 7 , 8 , 9 , 10 ]. Water flooding is one of the common development methods for conglomerate reservoirs, but long-term water flooding can form a high permeability water-flow channel between injection and production wells during the high water cut period, which intensifies the heterogeneity of the reservoir, resulting in the inability to displace the remaining oil in the low permeability area, low water injection sweep coefficient, much remaining oil, and inefficient or ineffective injection water circulation [ 11 , 12 , 13 ].…”
Section: Introductionmentioning
confidence: 99%
“…Organic-rich shales are crucial unconventional reservoirs for liquid and gaseous hydrocarbons . Large quantities of nanoscale pores , and micro/submillimeter-scale pores , occur in shales, providing appreciable storage space for free and adsorbed gas. , Pores in organic-rich shales are small and have poor connectivity. , The formation and evolution of pores are controlled by deposition/diagenesis of shales, organic matter maturation, and hydrocarbon generation/expulsion. Compared to inorganic pores, organic pores have a more significant role for storing hydrocarbon gases in shale reservoirs. The type, abundance, and maturity level of organic matter as well as the degree of oil cracking have important influences on the occurrence of organic pores in shales. ,, Many studies have characterized pore structures of shale reservoirs with multiple techniques, including N 2 and CO 2 adsorption, mercury penetration, nano-CT, and SEM observation. ,,, These works contribute significantly for shale gas exploration. However, it is difficult to quantitatively investigate organic and inorganic pores independently with respect to the total space and size of pores using conventional techniques. , For example, proportions of organic pores can be underestimated using the FE-SEM technique due to its limited spatial resolution and the inappropriate selection of the area of interest.…”
Section: Introductionmentioning
confidence: 99%