ON THE FORMATIVE MECHANISM OF THE ANOMALY HIGH-PRESSURE IN THE CARBONATE ROCK SYSTEM OF THE SICHUAN BASIN

Du Fengqin

doi:10.11781/sysydz199203296

Volume 14 Issue 3

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Du Fengqin. ON THE FORMATIVE MECHANISM OF THE ANOMALY HIGH-PRESSURE IN THE CARBONATE ROCK SYSTEM OF THE SICHUAN BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1992, 14(3): 296-301. doi: 10.11781/sysydz199203296

Citation:

Du Fengqin. ON THE FORMATIVE MECHANISM OF THE ANOMALY HIGH-PRESSURE IN THE CARBONATE ROCK SYSTEM OF THE SICHUAN BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1992, 14(3): 296-301. doi: 10.11781/sysydz199203296

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ON THE FORMATIVE MECHANISM OF THE ANOMALY HIGH-PRESSURE IN THE CARBONATE ROCK SYSTEM OF THE SICHUAN BASIN

doi: 10.11781/sysydz199203296

Du Fengqin

Southwest China Bureau of Petroleum Geology, MGMR

Received Date: 1989-07-05
Publish Date: 1992-07-25

Abstract

Abstract

The author of this paper describes the anomaly high-pressure in the Triassic and the Permo-Carboniferous systems based on the features of the carbonate diagenesis combined with the geological structures, sedimentary characters, petroleum evolution and the exploration practice in the Sichuan Basin. It is concluded that the high-pressure results from various geological actions during the stage of petroleum generation, migration and accumulation in the basin.