2019
DOI: 10.1016/j.ptlrs.2019.04.002
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Reservoir and development characteristics of the Da'anzhai tight oil in Sichuan Basin, SW China

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Cited by 4 publications
(3 citation statements)
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“…Combined with the results of high-pressure mercury intrusion experiment, for limestone formation, the percentage of micron-and submicron-scale pores has a tendency to increase as permeability increases, but the nanoscale pores still account for a large proportion. While the main contribution to permeability is derived from the micron-and submicron-scale pores, the fluid storage does not match the flow space, resulting in high resistance gradient (Wang et al 2019;Qiao et al 2020;Zhang et al 2020).…”
Section: Resultsmentioning
confidence: 99%
“…Combined with the results of high-pressure mercury intrusion experiment, for limestone formation, the percentage of micron-and submicron-scale pores has a tendency to increase as permeability increases, but the nanoscale pores still account for a large proportion. While the main contribution to permeability is derived from the micron-and submicron-scale pores, the fluid storage does not match the flow space, resulting in high resistance gradient (Wang et al 2019;Qiao et al 2020;Zhang et al 2020).…”
Section: Resultsmentioning
confidence: 99%
“…The shelly limestone is a kind of unique lithology in the Da'anzhai member, which is different from other formations. Partial shelly limestone in the Da'anzhai member, which has a high argillaceous content and high oil and gas production, can be considered as a source rock [23,24]. The Da'anzhai member is vertically characterized by a complete transgression-retrogression sedimentary cycle.…”
Section: Geologic Settingmentioning
confidence: 99%
“…In China, tight oil resources are mainly distributed in the Ordos Basin, Sichuan Basin, and Songliao Basin [7][8][9][10][11]. For example, the tight oil resources are abundant in the Taiyuan formation in the Ordos Basin and the Jurassic Da'anzhai Member in the Sichuan Basin, which are the typical lacustrine carbonate tight oil resources [12,13]. The tight limestone reservoir space of the Taiyuan formation is mainly composed of dissolution pores, residual organism cavities, intergranular pores, and microfractures, and the development of such reservoirs is mainly controlled by sedimentary microfacies, quasi-syngenetic karstification, and fractures, whereas the tight limestone reservoirs in the central Sichuan Basin are controlled by dissolution and tectonic processes [14], and the porosity and permeability of tight limestone are related to the calcite content [15].…”
Section: Introductionmentioning
confidence: 99%