TY  - SER
AU  - Liu,Yifeng
AU  - Qiu,Nansheng
AU  - Xie,Zengye
AU  - Yao,Qianying
AU  - Zhu,Chuanqing
TI  - Overpressure compartments in the central paleo-uplift, Sichuan Basin, southwest China
PY  - 2016///
CY  - 
PB  - 
N2  - Transcripción del resumen del autor: The Sichuan Basin is a prime gas-producing basin in China. Besides the giant Neoproterozoic Weiyuan gas field discovered in the central paleo-uplift, an extra giant gas reservoir in the Cambrian in this area has been confirmed in recent years. Although the lower Paleozoic in the southwest (Weiyuan area) is normally pressured, it is overpressured in the central area (Moxi–Gaoshiti area). Combined with the seal distribution, five pressure systems, including three overpressure systems, can be divided based on drill-stem test, mud weight, and sonic transit time data. Overpressures appear at depth interval of 1500 to 4900 m (4921 to 16,076 ft), approximately. Benefiting from the good sealing capacity of the gypsum in the Upper and Middle Triassic, high overpressure (pressure coefficient [r] > 2.0) has been preserved in the Lower Triassic, and the Upper Triassic and Cambrian are moderately overpressured (1.3 r
ER  -