Abstract
Natural gas exploration in the Middle Triassic Leikoupo Formation (T2l) in the Sichuan Basin of China has achieved a remarkable breakthrough in recent years and thus attracts wide attention. However, there is no consensus on the gas source. The genetic identification and gas–source correlation based on the geochemical characteristics of natural gas indicate that the natural gas in the Leikoupo Formation is mainly from the underlying Upper Permian Longtan/Wujiaping Formation (P3l/P3w) source rocks (Moxi). Nevertheless, it has assistance (Zhongba) or hydrocarbon supply condition (Chuanxi) brought by the source rocks in the 1st Member of the Upper Triassic Xujiahe Formation (T3x), or mainly from the T3x source rocks with a specific contribution by the T2l source rocks (Yuanba and Longgang). The T2l gas pools display three types of source-reservoir assemblages, and they suggest different exploration directions. The P3l source rocks serve as main source rocks that can constitute the lower-generation and upper-accumulation pattern. The positive structures around the deep faults connecting the P3l and T2l are the most favorable areas to explore large-scale T2l gas pools. The source rocks at the bottom of T3x and the reservoirs at the top of the T2l can constitute the side-generation and side-accumulation pattern, which is favorably developed in the residual karst hills or the local tectonic high position of the karst slope. The T2l can constitute self-generation and self-accumulation pattern, which assists in the formation of gas pools.
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