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富顺场构造所处的大地构造位置为川北古中拗陷低缓褶皱带东斜坡。在川北古中拗陷的西北侧为龙门山推覆构造带,东北为米仓山构造带。区内沉积构造经历了加里东～海西期的克拉通盆地、印支早期的被动大陆边缘、印支中期以后的前陆盆地演化阶段。该区资源可靠、构造基本落实、生出盖组合好、海相陆相兼备,三叠、侏罗系有多套储层,深浅同有、原生、次生并存,具有丰富的勘探开发价值。
The structure of the earth where the Fusun structure is located is the eastern slope of the low-lying fold belt in the middle-deep depression of North Sichuan. On the northwestern side of the middle-deep depression in North Sichuan, it is the Longmen Shan nappe tectonic belt and the northeast is the Micangshan tectonic belt. The sedimentary structures in the area have experienced the evolution of the Caledonian basin from Caledonian to Hercynian, the passive continental margin from the Early Indosinian, and the evolution of the foreland basin after the Indosinian period. The area has reliable resources, basically completed structures, good combination of cover formation and marine terrestrial facies. There are several sets of reservoirs in the Triassic and Jurassic, with the same depth and the same primary and secondary occurrences, and is rich in exploration and development value.