lower tertiary source rocks 第三系烃源岩
The gas of QHD30 1 is mixed gas and mainly from the coal derived gas from pre Tertiary source rocks.
QHD3 0 1气藏的天然气属多源混合气,主气源为前第三系的煤成气。
So compaction is not the main mechanism of hydrocarbon expulsion of the Low Tertiary source rocks in the Dongying Depression.
因此,压实排烃不是东营凹陷下第三系烃源岩排烃的主要机制。
The natural gas of the main type in North China Basin is generated in the symbiotic window of oil and gas in Lower Tertiary source rocks.
华北盆地天然气的主要类型是下第三系源岩在油气共生窗中生成的。
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