Research Article

Early Paleozoic Extension-Compression Transition and Formation of a Paleo-Oil Reservoir System in the NW Sichuan Basin: Implications for Deeply Buried Hydrocarbon Accumulation

Figure 13

(a) The inclusion Th of the Dengying Fm is 167–176°C. The Qixia Fm has two sets of peaks at 115–125°C and 135–145°C, respectively. (b) Thermal burial evolution that is combined with and fluid inclusion characteristics indicates that the gas (oil-cracked) charging period of the NSWSCD that mainly occurred in the Middle-Late Triassic to Early Jurassic.