指热催化作用下，有机质能够大量转化为石油和湿气的生油时期。既是有机质大量生成液态石油的温度(或深度)区间。
... oilgear 油压传动 oil-generating window 生油窗 oil-generative assemblage 生油层系 ...
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... generative kerogen 生油干酪根 generative window 生油窗 generator drive 发电机传动 ...
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所以在热催化作用下，有机质能大量转化为石油和湿气，俗称为“生油窗”（oil window）。有机质成熟的早晚还与其本身性质有关，如相同条件下，树脂体和高含硫的海相有机质成熟较早、藻质体生烃能力最强
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生油液态窗 liquid window of oil generation
侏罗系烃源岩地表处于低成熟油气生成阶段，覆盖区在生油窗之内，为现实烃源岩。
They are at mature to highly mature stage in Kekeya and Pusha-Keliyang areas, as practical hydrocarbon source rocks.
在生油窗内同一套烃源岩样品的ETR随深度（成熟度）增加无明显变化，具有很好的热稳定性；
There was no change in ETR of each source rock interval with the increase of depth in the oil window, which indicated ETR had excellent thermic stability.
下古生界烃源岩在西部坡折带及南北隆起区现今仍处于有效生油窗内（镜质组反射率小于1.3 % ）。
Nowadays, at the western slope and the northern and southern uplifts the Lower Paleozoic source formations are still in the active oil generation Rold ( R o< 1.3%).
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