收稿：2020-03-23，
纸质出版：2020-10-28
移动端阅览
综合运用油气地球化学分析方法，分析了渤海湾盆地渤中19-6凝析气田天然气成因，并对凝析油与天然气的成因关系进行了判识。研究结果表明，渤中19-6凝析气田天然气为以烃类气为主的湿气，C
1
/（C
2
+C
3
）值偏低，介于6.4~7.3，甲烷碳同位素值集中分布于-38.0‰~-39.0‰，乙烷碳同位素偏重，介于-25.4‰~-27.0‰，为偏腐殖型干酪根裂解气，与沙河街组三段烃源岩具有可比性，源自沙河街组三段烃源岩。多项凝析油和天然气成熟度判别参数表明，渤中19-6凝析气田凝析油和天然气主要处于成熟阶段，但天然气成熟度略高于凝析油。多项地质证据表明，渤中19-6凝析气田经历了“早油晚气”的油气成藏过程，凝析油主成藏期（12 Ma以来）早于天然气（5 Ma以来）。
The genesis of natural gas in the Bozhong 19-6 gas condensate field in the Bohai Bay Basin is analyzed by means of petroleum geochemical analyses
and the genetic relationship between condensate and natural gas is thereby determined.The results show that the natural gas in the Bozhong 19-6 gas condensate field is mainly composed of wet hydrocarbon gases with relatively low C
1
/(C
2
+C
3
) values ranging from 6.4 to 7.3
and carbon isotope values of methane and ethane ranging from -38.0‰ to -39.0‰ and from -25.4‰ to -27.0‰
respectively
indicating humic-prone kerogene-cracked gases probably derived from the s
ource rocks of the third member of the Shahejie Formation.A number of condensate and gas maturity parameters show that both condensate and natural gas from the field are mature
with natural gas slightly maturer than condensate.Geological evidences also reveal that the field went through a hydrocarbon accumulation process of "early oil and late gas"
with the main condensate accumulation stages (since 12 Ma) prior to those of natural gas (since 5 Ma).
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