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塔里木盆地下古生界海相高成熟生油岩干酪根仍具有一定的生烃潜力，其产烃率－温度－时间关系研究表明，在最近１－２Ｍａ内凹陷区奥陶系生油岩向邻近的隆起区提供了大量烃类。
The Lower Paleozoic marine marine karst kerogen in the Tarim Basin still has certain potential for hydrocarbon generation. Studies on its hydrocarbon-generation-temperature-time relationship indicate that the Ordovician source rocks in the recent 1-2Ma depression Adjacent uplifts provide a large amount of hydrocarbons.